#: locale=en

## Action

### PDF
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PopupPDFBehaviour_68AAC66D_7EFC_A279_41CA_6080A464226F.url = files/Chawchai%20et%20al.,%202021_en.pdf
PopupPDFBehaviour_0527923B_2E5D_823C_4191_799722C5F7DC.url = files/Chawchai%20et%20al.,%202021_en.pdf
PopupPDFBehaviour_0527E238_2E5D_823C_41C7_737547E453CA.url = files/Chawchai%20et%20al.,%202021_en.pdf
PopupPDFBehaviour_698E58DF_7EEB_AE59_41DF_41793D0DF650.url = files/Tan%20et%20al.,%202019_en.pdf
PopupPDFBehaviour_0526D236_2E5D_8234_4185_4AA608F9548B.url = files/Tan%20et%20al.,%202019_en.pdf

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## E-Learning

### Answer
questionOption_59F0DFCE_4F67_A486_41B9_5B157FDCE239.text = Argon
questionOption_59C10905_4F62_AD7B_4196_58845CBB050B.text = Bacterial
questionOption_5C3E0912_4F65_ED99_41A3_EA9A880EB901.text = Bat
questionOption_59C6E91E_4F63_AD86_41B6_DF9C4B78F71A.text = Bat bones
questionOption_5C3EF911_4F65_ED9B_419F_38435B1B2375.text = Bird 
questionOption_59B27C7D_4F66_EB8B_41D0_F1A867102D0D.text = Calcite 
questionOption_59C13905_4F62_AD7B_41B2_BC43FC952215.text = Capillary forces
questionOption_59F32FCE_4F67_A486_41D2_FFC9D78658A8.text = Carbon dioxide
questionOption_59CBF4BB_4F67_648E_41A9_8B9F02E3E258.text = Carbonic acid
questionOption_59CB14BB_4F67_648E_41B0_2A138FF7E51D.text = Carbonous acid
questionOption_59CB04BB_4F67_648E_41CF_91152FC4F958.text = Carboxylic acid
questionOption_5C4CD4A4_4F65_64BA_41AE_1545C979BA6B.text = Cave bacon
questionOption_57C03BBB_4F6D_AC8E_41BB_4C5E010AE9E6.text = Cave pearls
questionOption_B6539165_AA65_1267_41D9_AA97AD04F242.text = Cave pearls
questionOption_B2FC5D45_AA63_33A6_41DD_3777795781A4.text = Cave pearls
questionOption_8FB27E4B_AA65_11A3_41D5_D4F99821F604.text = Cave pearls
questionOption_5994C774_4F63_A59A_419D_069EFD6E0A91.text = Cave popcorn
questionOption_8FB20E4B_AA65_11A2_41DE_9770E328B730.text = Cave popcorn
questionOption_B5990B4C_AA7D_17A5_41B1_7A957BAD9AF9.text = Cave popcorn
questionOption_59DCC872_4F62_AB9E_41CC_529AF6ADA8B4.text = Cave popcorn
questionOption_B2FC0D45_AA63_33A6_41D7_1D3EC3A3911C.text = Columns
questionOption_57729793_4F62_E49E_41CD_30E54A9A3453.text = Columns
questionOption_59FB7C2F_4F7D_6B86_41B9_214D4AABA7E5.text = Columns
questionOption_59BA011F_4F63_9D86_4190_714756249706.text = Columns
questionOption_59EE83D3_4F62_9C9F_41C7_9352A473C867.text = Columns
questionOption_59C887A8_4F7D_A48A_41D1_EF403A08B21C.text = Columns 
questionOption_59CB90AD_4F63_BC8A_41C2_EA655E24D66B.text = Columns 
questionOption_59C789F1_4F65_EC9A_41D0_C27BEED30F5E.text = Coral 
questionOption_5C4CF4A4_4F65_64BA_41CE_F06C0B12D6F1.text = Coralloids
questionOption_8FB21E4C_AA65_11A5_41D5_00B445065572.text = Coralloids
questionOption_5721B272_4F6D_7F99_41CE_A1478FF3EE42.text = Coralloids
questionOption_B59EDB4C_AA7D_17A5_41A9_6E69BA95E364.text = Coralloids 
questionOption_59FCFB45_4F65_ADFA_41D0_8D786CC58ACF.text = Cubical
questionOption_59FB5C2F_4F7D_6B86_41C4_71E5E3C206F3.text = Curtain
questionOption_740C34BE_5A02_4CDC_41A6_E71D01180DEE.text = Curtain
questionOption_59E9645F_4F62_BB87_41D2_606E8B179215.text = Curtain
questionOption_59CA70AD_4F63_BC8A_41CC_3180AE58BED0.text = Curtain
questionOption_57BD7D7C_4F65_658A_41AB_4E30F9855539.text = Curtain
questionOption_88BDED1C_AA7D_73A5_41E3_716C712E3624.text = Curtain 
questionOption_59FCCB45_4F65_ADFA_41C1_0F6019CB7D4C.text = Cylindrical
questionOption_59B26C7D_4F66_EB8B_41D1_F60619BDBC2C.text = Dolomite 
questionOption_59C8A7A9_4F7D_A48A_41B3_9CC7283FDD36.text = Drapery
questionOption_59C9A0DA_4F62_9C8E_41BB_EB49703F57AB.text = Drapery
questionOption_740C44BE_5A02_4CDC_41C7_B1A038CC7E5D.text = Drapery 
questionOption_59FB6C2F_4F7D_6B86_41C6_7CDABC93F9B1.text = Drapery 
questionOption_88BDCD1D_AA7D_73A7_41DC_B34CCCA263D8.text = Drapery 
questionOption_585A1AE8_4F62_AC8A_41D0_9D726068EE13.text = Early Carboniferous
questionOption_585A0AE8_4F62_AC8A_41C9_C0BCE9AAEDD8.text = Early Permia
questionOption_577908E1_4FA3_ECBB_41B6_23E54E93935F.text = Early to Middle Permian
questionOption_57F328D0_4F5D_6C9A_41C9_C524367BE229.text = Fish 
questionOption_59C9C0DA_4F62_9C8E_41B0_62CE40AA47A1.text = Flowstones
questionOption_59C977A8_4F7D_A48A_41CB_3E5E0C8E3D38.text = Flowstones
questionOption_563892B7_4FA6_FC86_41BF_74CCE5CDC776.text = Flowstones
questionOption_B653C166_AA65_1265_41DA_1AFB6D42E202.text = Flowstones
questionOption_59F5516F_4F66_9D86_41CA_3DB43ECA42AB.text = Flowstones
questionOption_56FA3003_4FA2_9B7D_41C7_CBE0936E4B3B.text = Flowstones
questionOption_57CCE785_4F6F_657A_41D1_B907234A14BA.text = Flowstones
questionOption_59EE63D3_4F62_9C9F_41A4_E7358603C539.text = Flowstones 
questionOption_5C4CC4A4_4F65_64BA_41C7_D8360A00278E.text = Flowstones 
questionOption_571B3599_4F5D_E48A_41B3_C00A4037F901.text = Flowstones 
questionOption_59C9D0DA_4F62_9C8E_41CC_650C3181D258.text = Frostwork
questionOption_B5992B4C_AA7D_17A5_41DC_0BB2C7203869.text = Frostwork
questionOption_59F57170_4F66_9D9A_41BD_28E5E36EB5AA.text = Frostwork
questionOption_740C54BE_5A02_4CDC_41B7_06EFE3ED1977.text = Frostwork
questionOption_8FB23E4C_AA65_11A5_418B_68A31A85BC62.text = Frostwork 
questionOption_59C1A9BA_4F65_6C8E_41B8_8BDDC54D1176.text = Frostwork 
questionOption_59B21C7D_4F66_EB8B_41D3_90C7FC002178.text = Gypsum
questionOption_59B20C7D_4F66_EB8B_41B9_5FF5FAFB27C9.text = Halite
questionOption_88BD3D1D_AA7D_73A7_41BB_749489EEF9BD.text = Helictites
questionOption_59C897A8_4F7D_A48A_4183_50E14060CE47.text = Helictites
questionOption_B653A166_AA65_1265_41E3_3D13A1EBD2E9.text = Helictites
questionOption_740C04BE_5A02_4CDC_41BF_6387DEFDF59C.text = Helictites 
questionOption_59C980DB_4F62_9C8E_41D2_454A688B72C6.text = Helictites 
questionOption_567A10B0_4F62_9C9A_41B2_C56332169733.text = Helictites 
questionOption_59F56170_4F66_9D9A_419D_49D53C10AA16.text = Helictites 
questionOption_59DCD872_4F62_AB9E_41AE_F01C8972A171.text = Helictites 
questionOption_B59ECB4C_AA7D_17A5_419E_C6570E7FD85A.text = Helictites 
questionOption_59FCEB45_4F65_ADFA_41CF_7672BBCA7E42.text = Hexagonal
questionOption_5770F1E5_4FA5_BCBA_41C6_A8A82C441916.text = Hydrogen
questionOption_59E9545F_4F62_BB87_418B_39FEDB6AE135.text = Krabi Province
questionOption_59DCA871_4F62_AB9A_41C6_ABAAA8791B48.text = Krabi Province
questionOption_6035268C_562D_F217_41BF_37D7C556E144.text = Krabi Province
questionOption_59CD64A2_4F65_64BE_41BF_5E64E3BC6A94.text = Lampang
questionOption_585A3AE8_4F62_AC8A_41C0_881691D23F9E.text = Late Carboniferous
questionOption_585A6AE8_4F62_AC8A_4190_E162BCC87618.text = Middle to Late Permian
questionOption_59DCB871_4F62_AB9D_41D2_DFF51561DED6.text = Moonmike
questionOption_B5993B4C_AA7D_17A5_41DC_BFD3A331FF55.text = Moonmilk
questionOption_740C24BE_5A02_4CDC_41A3_58781C389EE0.text = Moonmilk
questionOption_88BDDD1C_AA7D_73A5_41CD_2B87D25E12F8.text = Moonmilk
questionOption_947DA84E_AAA3_11A2_41E0_E8980B38E20A.text = Not every stalactite has a complementary stalagmite, and many stalagmites may have no stalactites above them.
questionOption_59F33FCE_4F67_A486_41D1_F15E9617E63F.text = Oxygen
questionOption_59E9445F_4F62_BB87_41D0_0AAEFF673FBA.text = Phangnga Province
questionOption_6035368C_562D_F217_41A0_EEAD4504595F.text = Phangnga Province
questionOption_59CD54A2_4F65_64BE_41D2_C92D19321718.text = Phuket
questionOption_59C11905_4F62_AD7B_41CC_81BD4674EF2A.text = Piezoelectric forces
questionOption_59CD74A1_4F65_64BA_41CA_6E4F6B148A0A.text = Ratburi 
questionOption_B653D166_AA65_1265_419A_D7A4B5F5702E.text = Rimstone dams
questionOption_8FB22E4C_AA65_11A5_41CA_6B72EABB6024.text = Rimstone dams
questionOption_59FB4C2F_4F7D_6B86_41C5_419BDF35FA5A.text = Rimstone dams
questionOption_88BD2D1D_AA7D_73A7_41DC_B54DD341CE66.text = Rimstone dams
questionOption_59C6F91E_4F63_AD86_41CA_325487F066A0.text = Sand grains
questionOption_6035568C_562D_F217_41A5_698A8394629B.text = Satun Province
questionOption_5C3E7912_4F65_ED99_41CE_572E995ED078.text = Snake
questionOption_59C6991E_4F63_AD86_41D0_5F11163AB83D.text = Soda straw fragments
questionOption_59C189BA_4F65_6C8E_41CC_59287CCBA21F.text = Soda straws
questionOption_B2FC1D45_AA63_33A6_41E1_3317BCCBF7CB.text = Soda straws
questionOption_5994B773_4F63_A59E_41D0_DEC6AC3B356F.text = Soda straws
questionOption_59BA711F_4F63_9D86_41CE_35E04C2D6F08.text = Soda straws
questionOption_5389196A_4FA2_AD8E_41C3_A4B33D3BD548.text = Soda straws
questionOption_575A51B1_4F63_9C9A_413F_C1B36C47F378.text = Soda straws
questionOption_566E7A35_4F67_AF9A_41BC_DF8063EA247C.text = Soda straws 
questionOption_59FC9B45_4F65_ADFA_41D3_367D0239C958.text = Spherical 
questionOption_5C3E6912_4F65_ED99_41D2_855A0E41ED8F.text = Spider
questionOption_5994D774_4F63_A59A_419D_20DB19D070D5.text = Stalactites
questionOption_59E9745F_4F62_BB87_4198_68365DBB54C8.text = Stalactites
questionOption_59C1C9BA_4F65_6C8E_41AF_8E50BC6EE955.text = Stalactites
questionOption_59F5416F_4F66_9D86_41A4_9D9C5B7157E7.text = Stalactites
questionOption_59CA40AD_4F63_BC8A_418A_EDD8DA0E3459.text = Stalactites 
questionOption_59BA511E_4F63_9D86_41BD_4A90AD7BE31D.text = Stalactites 
questionOption_5C4CE4A4_4F65_64BA_417E_5E55C75DFA1D.text = Stalactites 
questionOption_59EE93D3_4F62_9C9F_41BF_03B52273B53B.text = Stalactites 
questionOption_B2FC3D45_AA63_33A6_41AF_6F20B4752DA7.text = Stalactites 
questionOption_947DD84E_AAA3_11A2_41D6_D5469DD24073.text = Stalactites are typically larger in diameter than stalagmites above them, and they have rounded tops rather than pointed tips.
questionOption_B2FC2D45_AA63_33A6_41E5_4C8395A7DABE.text = Stalagmites
questionOption_59C1D9BA_4F65_6C8E_41D3_7992B715FB1F.text = Stalagmites
questionOption_5994F774_4F63_A59A_41BC_3C3C1FE2D513.text = Stalagmites 
questionOption_59BA611E_4F63_9D86_41C2_73860CA4A267.text = Stalagmites 
questionOption_59CA50AD_4F63_BC8A_41CA_141BC47F5CC2.text = Stalagmites 
questionOption_59EE73D3_4F62_9C9F_4199_F8A3D0809C85.text = Stalagmites 
questionOption_947DC84E_AAA3_11A2_41DA_3B2F5F48690F.text = Stalagmites are typically larger in diameter than stalactites above them, and they have rounded tops rather than pointed tips.
questionOption_947DB84E_AAA3_11A2_41AE_D58A440733EE.text = Stalagmites have central and hollow tubes same as stalactites.
questionOption_59F0CFCE_4F67_A486_41C6_3D96C2DD45E3.text = Sulfur dioxide
questionOption_59CBE4BB_4F67_648E_41B9_83E3A522DC4B.text = Sulfuric acid
questionOption_59C799F1_4F65_EC9A_41C7_A0B9395E0E13.text = Threads
questionOption_59CD84A1_4F65_64BA_41AC_0D88EDBF487E.text = Thung Song
questionOption_B653B166_AA65_1265_41D9_5E71C5784788.text = Trang Province
questionOption_6035468C_562D_F217_41D1_FDB48AE468EE.text = Trang Province
questionOption_59C7F9F1_4F65_EC9A_41C2_5C5BAF1A5ADA.text = Twigs
questionOption_59C12905_4F62_AD7B_41A9_D43EF5D15470.text = Wind 
questionOption_59C6891E_4F63_AD86_41D2_649B918E5031.text = Wood fragments
questionOption_59C7E9F1_4F65_EC9A_4196_A6F1E04704C9.text = Worms

### Question
question_59C059F1_4F65_EC9A_41C0_5FA5715CC55B.title = Helictite forms have been described in several types except, Which one?
question_5C3F1910_4F65_ED99_41D1_73D6E61D0DA7.title = Klang cave was formerly known in Thai as Tham Kang, What does Kang refer to? 
question_59CB54BB_4F67_648E_41D1_D6B0958612B5.title = Speleothems are formed by water. Rainwater percolates through the soil, absorbing carbon dioxide gas and producing weak ____.
question_59CDC4A1_4F65_64BA_41D1_4072814FDB78.title = The limestone in this area is in the ____ group, which is the name used to refer to the Permian sedimentary rock group.
question_88BE4D1C_AA7D_73A5_41CD_E7AF08043DA4.title = The slab-like flowstone that protrudes from the wall may be called ________.
question_5859AAE7_4F62_AC86_41BF_45D104DEA357.title = What age period is the limestone in this area?
question_B2F35D44_AA63_33A6_41C4_394B96F6DE1F.title = What are rock formations that hang from cave roofs?
question_59937773_4F63_A59E_41D1_1D6BDCB240B1.title = What are the pointed rock formations that grow from cave floors?
question_59FD0B45_4F65_ADFA_41C6_95DD0736AD60.title = What is the most common shape of the cave pearl?
question_59C14905_4F62_AD7B_41BF_F0DBFC1DCE89.title = What is the most likely hypothesis of how helictites form?
question_59FBAC2F_4F7D_6B86_41BC_E58E60AA8DF3.title = What is the name of the speleothems in this picture?
question_59DC6871_4F62_AB9A_41D2_6350D0C59147.title = What is the name of the speleothems in this picture?
question_59F5016F_4F66_9D86_41BE_F4AE8901FC24.title = What is the name of the speleothems in this picture?
question_59EE23D3_4F62_9C9F_41B7_651F9CABB22C.title = What is the name of the speleothems in this picture?
question_59BA911E_4F63_9D86_41CE_F55A2DEF07B5.title = What is the name of the speleothems in this picture?
question_5C4D24A4_4F65_64BA_41BB_9ADA61CC614F.title = What is the name of the speleothems in this picture?
question_740F84BD_5A02_4CDC_41C3_4BBEE759B62C.title = What is the name of the speleothems in this picture?
question_B59E4B4B_AA7D_17A3_41BB_6E655CA69BCC.title = What is the name of the speleothems in this picture?
question_59E9145F_4F62_BB87_41B0_A6E619BF19AC.title = What is the name of the speleothems in this picture?
question_59CA10AD_4F63_BC8A_41A9_988A7F7F65B8.title = What is the name of the speleothems in this picture?
question_59C900DA_4F62_9C8E_41C1_C5A75DBAAB89.title = What is the name of the speleothems in this picture?
question_59BDDC7D_4F66_EB8B_41C5_F55FFAB2516E.title = What minerals make up limestone?
question_6035B68B_562D_F211_41B7_83195BCCEFBF.title = Where is Klang cave located?
question_59F36FCE_4F67_A486_41B6_4951929850FB.title = Which gas played a crucial role in cave and speleothems formation?
question_59C5391E_4F63_AD86_41CE_23FFB80953FF.title = Which material can act as nuclei for cave pearl growth?
question_59C937A8_4F7D_A48A_41D3_7EB559D0DFBA.title = Which of the following Speleothem is the result of a stalactite and a stalagmite joining?
question_947C284E_AAA3_11A2_41A7_A137749A6D81.title = Which sentence about stalagmites and stalactites is true?
question_8FB29E4B_AA65_11A3_41E4_B818703175C2.title = Which speleothems form where there is some gradient and hence flow, over the edge of a pool?
question_59C109BA_4F65_6C8E_41A7_DA8817176A95.title = Which speleothems have a spiny appearance due to the acicular habit of aragonite?
question_B6501165_AA65_1267_41DB_DE6D7F6A87C4.title = Which speleothems show the form twisted in every direction, making it seem like they were grown in zero gravity?

### Question Screen
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### Report Screen
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quizScore_E3B0BC3B_ED85_DC0D_41D3_667195A9BCB3.questionsCorrect = Correct
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### Timeout Screen
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## Hotspot

### Text
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HotspotPanoramaOverlayTextImage_5A1D734A_569C_1B0D_41D1_5729E2B07D67.text = Emerald Pool Chamber
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HotspotPanoramaOverlayTextImage_5AA3ED2C_56B4_0F05_41BB_FDD41E0B5B30.text = Emerald Pool Chamber
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HotspotPanoramaOverlayTextImage_584FF537_559C_1F03_41C8_D186B7B64501.text = Emerald Pool Chamber
HotspotPanoramaOverlayTextImage_5A8B4C22_56EC_0D3D_41C5_A333F1E47FE1.text = Emerald Pool Chamber
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HotspotPanoramaOverlayTextImage_5A822CFF_56F4_0D03_4162_7FC70FD643A1.text = Emerald Pool Chamber
HotspotPanoramaOverlayTextImage_58ED7DFF_5594_0F03_41D1_2663E5F5D4A5.text = Emerald Pool Chamber
HotspotPanoramaOverlayTextImage_5B4FF856_56B4_3505_41A0_B142AA7898DB.text = Emerald Pool Chamber
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HotspotPanoramaOverlayTextImage_58C70BFE_5594_0B05_4193_331D3B9F13C9.text = Emerald Pool Chamber
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HotspotPanoramaOverlayTextImage_CDA5B7F5_DC9A_250C_4190_250A084C1266.text = Flowstones
HotspotPanoramaOverlayTextImage_A13F4B8D_E6C1_D4F2_41EA_CE6FE2D84A2E.text = Flowstones
HotspotPanoramaOverlayTextImage_CDE21503_DC9E_E504_41E5_6099B644B810.text = Flowstones
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HotspotPanoramaOverlayTextImage_9102A936_8AC6_0C00_41DD_703E34E1FA05.text = Flowstones
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HotspotPanoramaOverlayTextImage_A141E58B_E6C1_5CF6_41E7_90AB41EE80B4.text = Flowstones
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HotspotPanoramaOverlayTextImage_AF7A1B0D_8509_6FF6_41D0_71EE983D370E.text = Flowstones
HotspotPanoramaOverlayTextImage_5E612C31_55B4_0D1F_41CE_B4718FBDF12E.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_592C63E0_55F4_1B3E_41C4_B7F5B012774A.text = Great Wall Chamber
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HotspotPanoramaOverlayTextImage_5F5D6E27_4B94_0D02_41C2_D4E612D273D0.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_590BD691_55F4_3D1F_41BA_08760E61D5C9.text = Great Wall Chamber
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HotspotPanoramaOverlayTextImage_5C343965_4BAC_1707_41D1_03C1F61648ED.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5932BC19_5594_0D0F_41AC_700EA87E0297.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5BA63772_55EC_FB1D_41B2_B43D1EEA8BFC.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_723DF558_5A02_4DA4_41CB_2DD438FDF99F.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5DA0DFD5_4BAC_0B07_41BA_55C66EB8CC91.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5EE85F37_559C_0B03_41D0_6FFA609E9746.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5D4027F6_4B9C_1B05_416A_4D7AF77B6FDE.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5EED72FF_5593_F503_41D0_B4CC05F5F080.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5C0246AA_4B94_3D02_41B1_3C120BB7C513.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5E0CE193_5594_3702_41C7_D40E518161C5.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5F8DE6AD_4B94_3D06_41C4_5433289EAD3D.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5C7CA503_4BB4_1F03_41A6_690F1E25D53A.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5D67B51B_4BAF_FF03_41C2_86A0D8365E85.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5AC06838_56EC_350E_41B8_EB26E7E30EB5.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_590D247D_55FC_7D07_41BB_CF04DE80368C.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_58C0B554_4BAC_1F06_41CB_6A8E4186A0C5.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5E23733D_55B4_1B07_41A4_90EB42E6A32A.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5E64740B_5594_1D03_418F_3493384FA53B.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5EA4A2F9_5594_350F_41BC_359217857806.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5D36C107_4B9C_3703_41C9_1F158379D1CD.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_596CFAED_55AC_1507_419F_6994DC5B1D30.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5D8673F7_4B94_1B03_419F_63766797937D.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5A25F89D_569C_3507_41C8_4E9DC5EA4FC4.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_592BAF78_56EC_0B0D_41B9_381FEF64ACB6.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5B0A0B6F_5694_0B03_41CD_C337485A207E.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5A3370AA_56AC_350D_41D1_5492E4F09E2E.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5E65DB46_4B94_0B05_4182_68CD2CF166E6.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5BA59E86_569C_0D05_41BC_ED3F188994AF.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_5EF5B63B_55B4_3D03_41CA_F2B39FDDBBD6.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_6648C8E3_56B4_7502_41D0_4FBEFDB6B1B1.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_59385A97_5594_1503_41CD_F14C4E72AB35.text = Great Wall Chamber
HotspotPanoramaOverlayTextImage_A1BAB601_E6C1_3FF5_41E5_2CE86A3C1098.text = Helictites
HotspotPanoramaOverlayTextImage_A19FBB2F_E6C3_540E_41E7_277F8CC79962.text = Helictites
HotspotPanoramaOverlayTextImage_407C9409_5C51_7668_41C0_E92E5DC94CB8.text = Hotspot
HotspotPanoramaOverlayTextImage_5BA199DA_56FC_170D_41B6_B1B5A068D4F4.text = Lake Entrance
HotspotPanoramaOverlayTextImage_586FB2CB_56F4_1503_41B0_FD45ED56A2FC.text = Lake Entrance
HotspotPanoramaOverlayTextImage_66B2D7B6_5694_3B05_419F_71A7FDE447A6.text = Lake Entrance
HotspotPanoramaOverlayTextImage_A609D43E_E6C1_7C0E_41C5_EF5BBAB348BD.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5B669B75_56B4_0B07_41CF_A27ABCD415CB.text = Lake Entrance
HotspotPanoramaOverlayTextImage_581A0176_56AC_F705_41C2_D155710A08D9.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5B7EBE31_56BC_0D1E_41CC_5572E0E6FAE6.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5A4C3B1C_569C_0B06_41AC_218AFC694CF7.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5AB20A20_56EC_153E_41B3_15227025CB09.text = Lake Entrance
HotspotPanoramaOverlayTextImage_58AA91BB_56F4_3702_41C8_2D0AA7AA38AD.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5AEDAA28_5694_750D_41CC_61B2B197DFF0.text = Lake Entrance
HotspotPanoramaOverlayTextImage_59652EA0_56F4_0D3D_41CE_F2E617308F85.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5BD182B7_56FC_1502_41CD_C026266DFBF9.text = Lake Entrance
HotspotPanoramaOverlayTextImage_58CAD976_56BC_F702_41B5_83CDF01F5840.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5A9A4FA7_56EC_0B02_41D0_600C87D4DE7F.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5B3E2C5C_56B4_0D05_4189_76C9E28D5582.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5B9F0E89_56AC_0D0F_41CC_D9053F679EF2.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5AB546F3_569C_3D03_41BD_BBC9275AFA92.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5B874951_56EC_171E_41BE_7E4E3F73A852.text = Lake Entrance
HotspotPanoramaOverlayTextImage_585A1285_5694_1507_41CC_3C9F35581651.text = Lake Entrance
HotspotPanoramaOverlayTextImage_585CA150_56B4_371D_41B7_F2504F716677.text = Lake Entrance
HotspotPanoramaOverlayTextImage_5F49E192_55FC_F702_41B1_140D4DDE1464.text = Large Chamber
HotspotPanoramaOverlayTextImage_5DFD8EFD_4B94_0D07_41B2_D0243E06107E.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E785937_4B9C_1702_41A0_F24EA83B4965.text = Large Chamber
HotspotPanoramaOverlayTextImage_5EB8D6A7_55FC_1D02_41C1_8D495D7D07C2.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E22015C_4BF4_1705_41CD_90D1C22E5A32.text = Large Chamber
HotspotPanoramaOverlayTextImage_5D818D1D_4BEC_0F07_41D0_E146EEC028DA.text = Large Chamber
HotspotPanoramaOverlayTextImage_5EAA0C16_55F4_0D05_41C4_A723C38677FB.text = Large Chamber
HotspotPanoramaOverlayTextImage_5F227DBE_55B4_0F05_419C_AE9E34C93EEB.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E8FEC6A_4BBC_0D0D_41B2_F056E2957078.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E937FEC_55EC_0B06_41CF_D8A1BF8A44C8.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E524AD6_5594_1502_41AD_DB037D012EB2.text = Large Chamber
HotspotPanoramaOverlayTextImage_5EA5CF6B_55FC_0B02_41BF_1A836ACD8CED.text = Large Chamber
HotspotPanoramaOverlayTextImage_59161195_5594_3706_41CB_E9769000F97F.text = Large Chamber
HotspotPanoramaOverlayTextImage_5B95C1CD_55B4_3707_41CE_0F7243310E5C.text = Large Chamber
HotspotPanoramaOverlayTextImage_5D80D3B6_4B94_1B05_4196_F59A339C5ACF.text = Large Chamber
HotspotPanoramaOverlayTextImage_5ED72587_5594_1F02_41C5_B765A2F14DC0.text = Large Chamber
HotspotPanoramaOverlayTextImage_5F44D421_55F4_1D3F_41CE_25EA6A982353.text = Large Chamber
HotspotPanoramaOverlayTextImage_5E7ABCB4_4B94_0D05_41BD_6ED8C68B9EB5.text = Large Chamber
HotspotPanoramaOverlayTextImage_5F4F523A_55F4_1502_41C6_8DB47630384B.text = Large Chamber
HotspotPanoramaOverlayTextImage_5EBBCAFA_55F4_7502_41A7_5576EBC66372.text = Large Chamber
HotspotPanoramaOverlayTextImage_5EA9CCF3_5594_0D03_41B5_39014BDE83E4.text = Large Chamber
HotspotPanoramaOverlayTextImage_5DD96208_4B94_350D_41B8_2968EA1A2075.text = Large Chamber
HotspotPanoramaOverlayTextImage_5C132A9E_4B94_3505_41C7_2C9F87956818.text = Large Chamber
HotspotPanoramaOverlayTextImage_5ED431A2_55AC_1702_41D0_7AB602A45772.text = Large Chamber
HotspotPanoramaOverlayTextImage_5CA2CCB4_4BEC_0D06_41CC_C613924ACBFE.text = Large Chamber 
HotspotPanoramaOverlayTextImage_5468EF66_4A9C_1399_41CA_07DAF4E6F917.text = Large Chamber 
HotspotPanoramaOverlayTextImage_5354A520_4BF4_3F3E_41C7_D2EA4EE24C55.text = Large Chamber 
HotspotPanoramaOverlayTextImage_5371DE45_4BF4_0D07_41D0_329DFDA913DE.text = Large Chamber 
HotspotPanoramaOverlayTextImage_5EF2B362_4BF4_3B3D_41C2_8F04B40FFD9B.text = Large Chamber 
HotspotPanoramaOverlayTextImage_54F2F38E_4AAC_72A9_41C6_939F3854A6B1.text = Large Chamber 
HotspotPanoramaOverlayTextImage_5DDFBA2A_4BF4_1502_41C3_B368FC3C4D37.text = Large Chamber 
HotspotPanoramaOverlayTextImage_549EC360_4A94_7399_41C7_043F63F84425.text = Parking Lot
HotspotPanoramaOverlayTextImage_54D800EA_4A94_0E69_41AA_E391471A2E45.text = Parking Lot
HotspotPanoramaOverlayTextImage_9C976505_8AC2_0400_41B5_72FA3EF99D98.text = Rimstone dams
HotspotPanoramaOverlayTextImage_90AEC2CD_8AFF_FC00_41CD_498E0957BA2D.text = Rimstone dams
HotspotPanoramaOverlayTextImage_CBCD5702_DC8E_2504_41D0_C3A98C681876.text = Rimstone dams
HotspotPanoramaOverlayTextImage_92E1B8C1_8AC2_0C01_41C7_0A0818EB5375.text = Rimstone dams
HotspotPanoramaOverlayTextImage_A13B7CB2_E6C3_4C17_41E0_DF87332668A4.text = Soda straw
HotspotPanoramaOverlayTextImage_CB48854F_DC8E_651C_41DE_96F875DD4EED.text = Soda straws
HotspotPanoramaOverlayTextImage_9F93817D_8AC2_3C00_41D6_C72A9939E4FB.text = Soda straws
HotspotPanoramaOverlayTextImage_9C3D1E05_8AC2_0400_41D3_3220C07D45A5.text = Soda straws
HotspotPanoramaOverlayTextImage_9E37B0EB_8AC2_1C00_41D6_1F7DC41056DC.text = Soda straws
HotspotPanoramaOverlayTextImage_92E9A4C9_8ADE_0401_41D6_DEA4BD8A89E6.text = Soda straws
HotspotPanoramaOverlayTextImage_A1FAC3CE_E6C3_F40F_41D9_06035A703425.text = Soda straws
HotspotPanoramaOverlayTextImage_CDE752A3_DC8E_1F0B_41EB_0323A5B4ECEC.text = Soda straws
HotspotPanoramaOverlayTextImage_9612E43F_8AC2_0400_41D1_C7C9E741EE7E.text = Soda straws \

HotspotPanoramaOverlayTextImage_A1A2429D_E6C1_340D_41DA_EE8A39761D7D.text = Stalacmite with     Cave Popcorn
HotspotPanoramaOverlayTextImage_915DB651_8AC2_0400_41D9_7AAD30531119.text = Stalactites
HotspotPanoramaOverlayTextImage_96ADA57C_8AC2_0407_41CD_28FF51267836.text = Stalactites
HotspotPanoramaOverlayTextImage_96D74FFF_8AFE_0400_41A9_E05C884F4554.text = Stalactites
HotspotPanoramaOverlayTextImage_CB673601_DC8A_2707_4171_D6D496AC669E.text = Stalactites
HotspotPanoramaOverlayTextImage_9734A95F_8AC2_0C00_41DC_C21B49123572.text = Stalactites
HotspotPanoramaOverlayTextImage_A0BE87E4_E6C1_FC32_41E0_07E39A944E4E.text = Stalactites
HotspotPanoramaOverlayTextImage_A3D9D1E3_E6C6_D436_41DD_334C8BFD5A69.text = Stalactites
HotspotPanoramaOverlayTextImage_9777DB11_8AC2_0C00_41D8_C7F89B3CE47E.text = Stalactites
HotspotPanoramaOverlayTextImage_9DB143BE_8AC3_FC03_41BD_BD212BEA525B.text = Stalactites
HotspotPanoramaOverlayTextImage_96E7B402_8AC2_0400_41D6_3967FCF4C199.text = Stalactites
HotspotPanoramaOverlayTextImage_962BF2BF_8AC2_3C00_41C9_5924239115E6.text = Stalactites
HotspotPanoramaOverlayTextImage_9656F284_8AC2_3C00_41AE_90AE6BC697E5.text = Stalactites
HotspotPanoramaOverlayTextImage_94093B8D_8AC2_0C00_41E0_C8938E66D25D.text = Stalactites
HotspotPanoramaOverlayTextImage_CD5CF2E8_DC9A_1F04_41D9_C2A309D02AA4.text = Stalactites
HotspotPanoramaOverlayTextImage_9238DD28_8AC6_0400_41CB_339901C9C1F4.text = Stalactites
HotspotPanoramaOverlayTextImage_9617D6E2_8AC2_0400_41D2_4AF3824DE4DC.text = Stalactites
HotspotPanoramaOverlayTextImage_91826C3F_8AC2_0400_41E0_11FB3F4D6A44.text = Stalactites \

HotspotPanoramaOverlayTextImage_90AF1497_8AC2_0400_4132_AD8D026D0EF8.text = Stalactites \

HotspotPanoramaOverlayTextImage_A0C4C5DC_E6C7_3C12_41DF_8A34B2773CED.text = Stalagmites
HotspotPanoramaOverlayTextImage_914AC535_8AFE_0400_41CF_FD5D8475E07E.text = Stalagmites
HotspotPanoramaOverlayTextImage_944F194B_8AC2_0C00_41DB_E1375F352B32.text = Stalagmites
HotspotPanoramaOverlayTextImage_A9BEBBE4_850B_6E36_41DB_16B6BB0702B6.text = Stalagmites
HotspotPanoramaOverlayTextImage_96A1B90C_8AC2_0C00_41CE_9737537BBD5B.text = Stalagmites
HotspotPanoramaOverlayTextImage_9176E565_8AC2_0400_41CA_8AE8F73CDDC6.text = Stalagmites
HotspotPanoramaOverlayTextImage_9694C1CB_8AC2_3C00_41DD_3137CBB92291.text = Stalagmites
HotspotPanoramaOverlayTextImage_A66285E0_E6C2_DC32_41D1_0AF2AB7207F7.text = Stalagmites
HotspotPanoramaOverlayTextImage_981914D2_8ACE_0400_41DF_AD3680F6AB72.text = Stalagmites
HotspotPanoramaOverlayTextImage_9BDE643D_8AC6_0400_41D7_FE92C4BF4BC9.text = Stalagmites
HotspotPanoramaOverlayTextImage_A1E85C85_E6C7_4CF2_41D9_5BFAEB473D65.text = Stalagmites
HotspotPanoramaOverlayTextImage_911A9A15_8AC2_0C01_41B9_D92468FBF8DC.text = Stalagmites
HotspotPanoramaOverlayTextImage_A14D35FC_E6C1_3C12_41A2_FD632AB4B1C0.text = Stalagmites
HotspotPanoramaOverlayTextImage_9E966888_8AC2_0C00_41DA_729D70447AD6.text = Stalagmites
HotspotPanoramaOverlayTextImage_917339BF_8AC6_0C01_41D5_376653E35A28.text = Stalagmites \

HotspotPanoramaOverlayTextImage_915C12A6_8AC6_1C00_41D3_F90C4248FD10.text = Stalagmites \

HotspotPanoramaOverlayTextImage_91723590_8AC6_0400_41C0_03CE0F2B9104.text = Stalagmites \

HotspotPanoramaOverlayTextImage_91F8D1EB_8AC6_FC00_41D4_1AB9AF112E6E.text = Stalagmites \

HotspotPanoramaOverlayTextImage_5C611828_4BAC_150D_41C9_70B0B76C5320.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5C2E5950_4BF4_171D_41CD_9D11A4B7095E.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5C3AD96A_4BF4_770D_41B0_DD840F04821C.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_514D749F_4B94_1D03_41CA_6FDAB17C8499.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_55522610_4AAC_35B9_41CD_AA7C26C54913.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5DF71948_4B94_170D_41AB_BE7C582F7937.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_548D5673_4AAC_327F_41BB_C4A10742CBD8.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5D0618C5_4BB3_F507_41CE_624E5B2008BA.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5DC7CE3D_4B94_0D07_419B_DF947F36DB94.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5C71A2CF_4BF4_1502_41B2_F3FD3350D77C.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5D85C8DB_4B94_1503_41BC_85AE29759A25.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5DC01EE5_4B9C_0D06_41C1_90BD8994F6B4.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_543FD3F8_4A94_326A_41C5_3FAFCF0639DC.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_531D2463_75E6_2CA6_41D7_5C1A54DC859A.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_5436AD61_4A94_379B_41B4_91333A5EAE1C.text = Tourist Entrance
HotspotPanoramaOverlayTextImage_55EDDDBA_4A94_16EE_41A1_18CC0962D1D6.text = Tourist Entrance \
 \

HotspotPanoramaOverlayTextImage_5E74D5F7_4BB4_3F02_41B2_E0BA3DAA59A4.text = Warning: This page contains a picture of a spider. Click to reveal.
HotspotPanoramaOverlayTextImage_7D626257_5A0E_47AC_4165_5FF452B53951.text = Warning: This page contains a picture of bats. Click to reveal.
HotspotPanoramaOverlayTextImage_7271F6F3_5A02_4C64_41CD_A9D6C149534C.text = Warning: This page contains a picture of millipedes. Click to reveal.
HotspotPanoramaOverlayTextImage_7D05F81A_5A02_C3A4_41C3_BABAA499492D.text = Warning: This page contains a video of a snake. Click to reveal.

### Tooltip
HotspotMapOverlayArea_CE40616D_EA8E_4404_41D2_B79A108C729A.toolTip = Buddha Images
HotspotMapOverlayArea_CF9CE7D2_EA8A_4C1C_41D3_2B2F72174DA0.toolTip = Coffee Straws Chamber
HotspotMapOverlayArea_CEE14017_EA86_4404_41E6_73E21D8FC59C.toolTip = Emerald Pool Chamber
HotspotMapOverlayArea_CF25E7F1_EA8D_CC1C_41BC_BA70F0B24BD3.toolTip = Great Wall Chamber
HotspotMapOverlayArea_CE33B901_EA8E_45FD_41E2_E4808689075E.toolTip = Lake Entrance
HotspotMapOverlayArea_33ABEF93_2526_ED39_41AA_1F10833E4915.toolTip = Large Chamber
HotspotMapOverlayArea_CE8F0E43_EA8E_DC7C_41E5_553DF6F9081B.toolTip = Tourist Entrance

## Media

### Audio
audiores_D41B4A14_E860_079F_41E2_9A8C479C47C9.mp3Url = media/audio_0071206F_2317_89B7_41AC_EC894597E0D7_en.mp3
audiores_4D1EA3FE_6CE7_9952_41DA_DC69272D280C.mp3Url = media/audio_4DE53371_6CE5_9951_41D5_3FAC566B0E78_en.mp3
audiores_AEAC8268_BB9E_BBAA_41E7_65D38B35527C.mp3Url = media/audio_609F8172_7D99_8972_41DB_3905B6069560_en.mp3
audiores_AEAC61A0_BB9E_B95A_41DF_19D4E9F169FD.mp3Url = media/audio_60D86D9B_7D99_B9B2_41DD_570789775418_en.mp3
audiores_B4235B87_BBA2_8965_41D6_5FB43D3DBEFB.mp3Url = media/audio_62385DF8_7D98_997E_41DD_C2E8989E8234_en.mp3
audiores_B4215951_BBA2_89FA_41D4_4FFFB57AAD9F.mp3Url = media/audio_6275BBF1_7D98_B98E_419B_59F525C769B4_en.mp3
audiores_B42727AB_BBA2_78AD_419C_3D9FE0C000BF.mp3Url = media/audio_62C6441D_7D98_8EB6_41D4_7A5030114B4D_en.mp3
audiores_AEBBC086_BB9E_B766_41E5_3A013D8FC484.mp3Url = media/audio_630D7C13_7D99_9EB2_41B3_ABF5D30C42BE_en.mp3
audiores_B42B6256_BBA2_9BE6_41E7_2C159A932984.mp3Url = media/audio_633859A8_7D99_799E_41D8_2CCE85E10F88_en.mp3
audiores_B42FFF5C_BBA2_89EB_41E6_937204B24CBC.mp3Url = media/audio_63A7DA0B_7D98_BA91_4190_C0BDA073CB0C_en.mp3
audiores_B42C8DFF_BBA2_88A5_41C4_C703B42CDD62.mp3Url = media/audio_63DDC82B_7D98_8692_41C8_DA53D0358B8E_en.mp3
audiores_AEABA330_BB9E_B9BA_41C7_FDD47D0EBA73.mp3Url = media/audio_6407C828_7D99_869E_41D7_64866A0488CD_en.mp3
audiores_A10C2FA0_E6C1_CC32_41E1_924724678D7F.mp3Url = media/audio_651E75CF_7D98_8992_41DF_1E9F3AFF30D9_en.mp3
audiores_C40DF8D3_E642_D416_41D3_98DF0A5AB8BC.mp3Url = media/audio_656BDC83_7D98_9F92_41CE_1DC638EA0F42_en.mp3
audiores_C434B51C_E642_DC12_41C4_1E5698B18CA1.mp3Url = media/audio_659EC956_7D98_86B2_41C1_C9FFED5BDC5F_en.mp3
audiores_B422DD06_BBA2_8967_41E1_2101BAA92AF1.mp3Url = media/audio_65B7B5F3_7D99_8972_41DB_2260B894288B_en.mp3
audiores_B4D8560B_BBA2_7B6E_41DF_C51F946FD48E.mp3Url = media/audio_7AFECD1C_6B95_3648_41BA_7D0952AC052C_en.mp3
audiores_B429807A_BBA2_97AF_41E0_CC2D6A611CA0.mp3Url = media/audio_AE11A7C1_8A21_F743_41C5_CCBCBF127B4D_en.mp3
audiores_C40B77D8_E642_DC12_41E2_24402D9BFCB4.mp3Url = media/audio_AE87B859_8A21_3942_41E0_DE691E9E3BDF_en.mp3
audiores_AEAAC3F7_BB9E_B8A5_41D7_95AA83B070CC.mp3Url = media/audio_AEE32A2F_8A21_78DF_41D7_BA4622210C34_en.mp3
audiores_C4012CCC_E642_CC72_4181_D512788978BF.mp3Url = media/audio_AF102EB8_8A21_59C1_4194_B7333DEF58DF_en.mp3
audiores_C400ABBF_E642_D40E_41DD_E4928E5B2731.mp3Url = media/audio_AF578705_8A21_28C3_41C7_4C38726438DC_en.mp3
audiores_C40E8A30_E642_D412_419B_716F71A73B3C.mp3Url = media/audio_AF921BA2_8A20_FFC6_41D6_6619831BA1C1_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3
audiores_4A27E277_5EC4_0A1F_41BB_EEB5031929A7.mp3Url = media/audio_E9EAF53B_D436_F3AD_41B0_022059FB461C_en.mp3

### Floorplan

### Image
imlevel_5159A23F_441D_CBDB_41B2_6E0D54F3856D.url = media/map_07432264_1470_5AE4_41AD_92127F8DB692_en_0.png
imlevel_5159C240_441D_CBA5_41BB_155BDDF6D348.url = media/map_07432264_1470_5AE4_41AD_92127F8DB692_en_1.png
imlevel_5159F241_441D_CBA7_41C6_01C43FEFFFFF.url = media/map_07432264_1470_5AE4_41AD_92127F8DB692_en_2.png
imlevel_5159E242_441D_CBA5_41D0_75A5A20BA4FB.url = media/map_07432264_1470_5AE4_41AD_92127F8DB692_en_3.png
imlevel_51593243_441D_CBAB_41C7_78A34B0572A8.url = media/map_07432264_1470_5AE4_41AD_92127F8DB692_en_4.png
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### Subtitle
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### Title
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album_42C18A06_7662_246E_41BB_812CC1541B37_0.label = Rim
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photo_64542F81_7C97_798E_41C7_8D2C51455311.label = correlation + explanation final
photo_65E4DF46_7C97_9A92_41C1_A66AAC1AA480.label = correlation + explanation final 2
album_4459880E_765D_E47E_41D5_0D9E41473228_0.label = flow
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### Video
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### Video Subtitles

## Skin

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### Image
Image_1B99DD00_16C4_0505_41B3_51F09727447A.url = skin/Image_1B99DD00_16C4_0505_41B3_51F09727447A_en.png
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### Label
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Label_3EE0DBDD_6C1A_8951_41D0_A36CE7E4F556.text = Click Image to see PDF
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Label_72C21040_6CE6_96AF_41D7_7063F9B85FE8.text = Go to 3D View
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Label_D9962573_F78E_CC1C_41D2_BF6A9B21D06B.text = INTRODUCTION
Label_492E9616_5013_FF0E_41C2_F21C9F5EEABD.text = KLANG CAVE, KRABI
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Label_0DD14F09_1744_0507_41AA_D8475423214A_mobile.text = KLANG CAVE, KRABI
Label_0DD14F09_1744_0507_41AA_D8475423214A.text = KLANG CAVE, KRABI
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Label_60AD4D33_4FA5_E59E_41B2_8A4476655B66.text = Panoramas without audio narration
Label_60AD4D33_4FA5_E59E_41B2_8A4476655B66_mobile.text = Panoramas without audio narration
Label_0C9A63CB_137B_F3BE_418D_7C157249586A_mobile.text = QUIZ COMPLETED : {{quiz.score1.questions.answered}}/{{quiz.score1.question.count}}
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Label_D8323A7F_E8A0_0789_41CF_42B64F231D52_mobile.text = เลือกภาษา

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HTMLText_69AAF5F3_5A02_4C6B_41C2_C8688116CFF2_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">The video was filmed in the hard-to-reach areas of Klang Cave that are not included in this virtual tour.</SPAN></SPAN></DIV></div>
HTMLText_4E37B3D6_59DD_6FA5_41BC_072196A389DA_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">The video was filmed in the hard-to-reach areas of Klang Cave that are not included in this virtual tour.</SPAN></SPAN></DIV></div>
HTMLText_054D6E42_105A_0ADB_418A_6BE331016811_mobile.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:3.28vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>G</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>eological </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>B</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>ackground</B></SPAN></SPAN></DIV><DIV STYLE="text-align:center;font-size:3.497267759562821vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">________________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Klang Cave is formed by the dissolution of Permian limestone within an isolated karst tower in Krabi Province, which is part of the Ratburi Group (orange and brown in the geological map). In this region, most inland karst towers and hills of Jurassic (blue) and Cretaceous (green) sedimentary rocks rise above Quaternary alluvial and colluvial plains forming a series of north-south ridges. Cretaceous granite (pink) is also distributed within this north-south structural trend of the Sibumasu tectonic block.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;"><B>Further reading</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Geological Map of Changwat Krabi (http://www.dmr.go.th/ download/00user/zoning/</SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';text-indent:17.7px;">แผนที่ธรณีวิทยาจังหวัดกระบี่</SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">.pdf)</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Harper, S. B., Morphology of Tower Karst in Krabi, Southern Thailand. Department of Geology, East Carolina University, Greenville, NC 27858,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Ridd, M.F., Barber, A.J., and Crow, M.J. (Eds), 2011. The Geology of Thailand. Geological Society, London</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Whaley, J., 2021. Geotourism: Thailand - Cliffs, Kayaks and Krabi. GEO ExPro. Vol. 18, No. 4 ( https://www.geoexpro.com/articles/2021/10/geotourism-thailand-cliffs-kayaks-and-krabi)</SPAN></SPAN></DIV></div>
HTMLText_054D6E42_105A_0ADB_418A_6BE331016811.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:3.28vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>G</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>eological </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>B</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>ackground</B></SPAN></SPAN></DIV><DIV STYLE="text-align:center;font-size:3.497267759562821vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">________________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Klang Cave is formed by the dissolution of Permian limestone within an isolated karst tower in Krabi Province, which is part of the Ratburi Group (orange and brown in the geological map). In this region, most inland karst towers and hills of Jurassic (blue) and Cretaceous (green) sedimentary rocks rise above Quaternary alluvial and colluvial plains forming a series of north-south ridges. Cretaceous granite (pink) is also distributed within this north-south structural trend of the Sibumasu tectonic block.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;"><B>Further reading</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Geological Map of Changwat Krabi (http://www.dmr.go.th/ download/00user/zoning/</SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';text-indent:17.7px;">แผนที่ธรณีวิทยาจังหวัดกระบี่</SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">.pdf)</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Harper, S. B., Morphology of Tower Karst in Krabi, Southern Thailand. Department of Geology, East Carolina University, Greenville, NC 27858,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Ridd, M.F., Barber, A.J., and Crow, M.J. (Eds), 2011. The Geology of Thailand. Geological Society, London</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.7px;padding-right:17.7px;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.7px;"><SPAN STYLE="color:#333333;font-size:1.64vmin;text-indent:17.7px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';text-indent:17.7px;">Whaley, J., 2021. Geotourism: Thailand - Cliffs, Kayaks and Krabi. GEO ExPro. Vol. 18, No. 4 ( https://www.geoexpro.com/articles/2021/10/geotourism-thailand-cliffs-kayaks-and-krabi)</SPAN></SPAN></DIV></div>
HTMLText_68559770_4FA5_6599_41CA_8BCA9B1BC46F_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>irtual </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>T</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>our</B></SPAN></SPAN></DIV><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.28vmin;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.09vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>About</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.77vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:2.185792349726775vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This virtual tour is part of the research project  " MAPPING KLANG CAVE USING 3D IMAGING LASER SCANNER AND GEOTOURISM DEVELOPMENT IN KRABI PROVINCE</SPAN><SPAN STYLE="color:#333333;font-size:2.19vmin;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">"</SPAN><SPAN STYLE="color:#333333;font-size:2.19vmin;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">funded by the Faculty of Science, Chulalongkorn University.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Funding</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.77vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Sci-Super VIII _65_006                                   </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Faculty of Science, Chulalongkorn University,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Phaya Thai Road, Wang Mai, Pathum Wan, Bangkok, 10330.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This research is also partly funded by Thailand Science Research and Innovation Fund Chulalongkorn University (DIS66230002).</SPAN></SPAN></DIV></div>
HTMLText_68559770_4FA5_6599_41CA_8BCA9B1BC46F.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>irtual </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>T</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>our</B></SPAN></SPAN></DIV><DIV STYLE="text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.28vmin;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.09vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>About</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.77vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:2.185792349726775vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This virtual tour is part of the research project  " MAPPING KLANG CAVE USING 3D IMAGING LASER SCANNER AND GEOTOURISM DEVELOPMENT IN KRABI PROVINCE</SPAN><SPAN STYLE="color:#333333;font-size:2.19vmin;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">"</SPAN><SPAN STYLE="color:#333333;font-size:2.19vmin;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">funded by the Faculty of Science, Chulalongkorn University.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Funding</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.77vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Sci-Super VIII _65_006                                   </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Faculty of Science, Chulalongkorn University,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Phaya Thai Road, Wang Mai, Pathum Wan, Bangkok, 10330.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.7486338797814225vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This research is also partly funded by Thailand Science Research and Innovation Fund Chulalongkorn University (DIS66230002).</SPAN></SPAN></DIV></div>
HTMLText_51461BAE_7942_7357_41D0_5B28F6703CB0_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Welcome to a virtual tour of Klang cave in Ao Luek District, Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand, and are well-known across Southeast Asia. This cave is around 1 km deep. There are 13 chambers and numerous types of speleothems.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This virtual tour is designed to allow visitors to view the cave's inside from the comfort of their own homes.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">In this virtual tour If you click on the red hotspot In the panorama, a quiz will appear on the screen. You can select multiple choices in the quiz. If you select the correct answer you will get 1 point, but if you select the wrong answer you will lose 1 point per each answer you select.</SPAN></SPAN></DIV></div>
HTMLText_51461BAE_7942_7357_41D0_5B28F6703CB0.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Welcome to a virtual tour of Klang cave in Ao Luek District, Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand, and are well-known across Southeast Asia. This cave is around 1 km deep. There are 13 chambers and numerous types of speleothems.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This virtual tour is designed to allow visitors to view the cave's inside from the comfort of their own homes.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:0.9950248756218927vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">In this virtual tour If you click on the red hotspot In the panorama, a quiz will appear on the screen. You can select multiple choices in the quiz. If you select the correct answer you will get 1 point, but if you select the wrong answer you will lose 1 point per each answer you select.</SPAN></SPAN></DIV></div>
HTMLText_513A596B_7942_5FDC_41CC_0E6B5858E59E.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>About</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.44vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.2515644555694605vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This virtual tour is part of the research project  " MAPPING KLANG CAVE USING 3D IMAGING LASER SCANNER AND GEOTOURISM DEVELOPMENT IN KRABI PROVINCE</SPAN><SPAN STYLE="color:#333333;font-size:1.25vw;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">"</SPAN><SPAN STYLE="color:#333333;font-size:1.25vw;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">funded by the Faculty of Science, Chulalongkorn University.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Funding</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.44vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Sci-Super VIII _65_006                                   </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Faculty of Science, Chulalongkorn University,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Phaya Thai Road, Wang Mai, Pathum Wan, Bangkok, 10330.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.56vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This research is also partly funded by Thailand Science Research and Innovation Fund Chulalongkorn University (DIS66230002).</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Acknowledgment</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Boitnoi Voice is thanked for providing AI voice generator.</SPAN></SPAN></DIV></div>
HTMLText_513A596B_7942_5FDC_41CC_0E6B5858E59E_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>About</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.44vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.2515644555694605vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This virtual tour is part of the research project  " MAPPING KLANG CAVE USING 3D IMAGING LASER SCANNER AND GEOTOURISM DEVELOPMENT IN KRABI PROVINCE</SPAN><SPAN STYLE="color:#333333;font-size:1.25vw;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">"</SPAN><SPAN STYLE="color:#333333;font-size:1.25vw;font-family:'Montserrat';"> </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">funded by the Faculty of Science, Chulalongkorn University.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Funding</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.44vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Sci-Super VIII _65_006                                   </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Faculty of Science, Chulalongkorn University,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Phaya Thai Road, Wang Mai, Pathum Wan, Bangkok, 10330.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.56vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">This research is also partly funded by Thailand Science Research and Innovation Fund Chulalongkorn University (DIS66230002).</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Acknowledgment</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Boitnoi Voice is thanked for providing AI voice generator.</SPAN></SPAN></DIV></div>
HTMLText_5192DC32_7942_D54C_41D4_F5E9B3477941_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">As the name implies, it often lives deep within caves where its diet consists mainly of bats. They have a yellow to beige background that darkens to a grey-black towards the tail. A white-to-cream mid-dorsal stripe starts about half of the way down the body and continues to the tip of the tail. Both sides of the head are marked just behind the eye with a black stripe surrounded by blue. Whilst non-venomous, this snake is known to be highly defensive and will readily strike and inflict a painful bite if approached too closely.</SPAN></SPAN></DIV></div>
HTMLText_5192DC32_7942_D54C_41D4_F5E9B3477941.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">As the name implies, it often lives deep within caves where its diet consists mainly of bats. They have a yellow to beige background that darkens to a grey-black towards the tail. A white-to-cream mid-dorsal stripe starts about half of the way down the body and continues to the tip of the tail. Both sides of the head are marked just behind the eye with a black stripe surrounded by blue. Whilst non-venomous, this snake is known to be highly defensive and will readily strike and inflict a painful bite if approached too closely.</SPAN></SPAN></DIV></div>
HTMLText_44358851_5A02_43A4_41BD_CB9E2DC6292A.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Heteropoda is a genus of spiders in the family Sparassidae, the huntsman spiders. They are mainly distributed in tropical Asia and Australia. These spiders catch and eat insects, but in a laboratory study, one species readily ate fish and tadpoles when offered. The largest species in the genus, H. maxima, is about 4.6 centimeters long but has a leg span of up to 30 centimeters, therefore being the largest of any extant spider.</SPAN></SPAN></DIV></div>
HTMLText_44358851_5A02_43A4_41BD_CB9E2DC6292A_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Heteropoda is a genus of spiders in the family Sparassidae, the huntsman spiders. They are mainly distributed in tropical Asia and Australia. These spiders catch and eat insects, but in a laboratory study, one species readily ate fish and tadpoles when offered. The largest species in the genus, H. maxima, is about 4.6 centimeters long but has a leg span of up to 30 centimeters, therefore being the largest of any extant spider.</SPAN></SPAN></DIV></div>
HTMLText_453DC955_5A02_45AC_41B6_FBFFD237BC48_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Megadermatidae, or false vampire bats, are a family of bats found from central Africa, eastwards through southern Asia, and into Australia. They are relatively large bats, ranging from 6.5 cm to 14 cm in head-body length. They have large eyes, very large ears, and a prominent nose-leaf. They have a wide membrane between the hind legs, or uropatagium, but no tail. Many species are a drab brown in color, but some are white, bluish-grey, or even olive-green, helping to camouflage them against their preferred roosting environments. They are primarily insectivorous, but will also eat a wide range of small vertebrates.</SPAN></SPAN></DIV></div>
HTMLText_453DC955_5A02_45AC_41B6_FBFFD237BC48.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Megadermatidae, or false vampire bats, are a family of bats found from central Africa, eastwards through southern Asia, and into Australia. They are relatively large bats, ranging from 6.5 cm to 14 cm in head-body length. They have large eyes, very large ears, and a prominent nose-leaf. They have a wide membrane between the hind legs, or uropatagium, but no tail. Many species are a drab brown in color, but some are white, bluish-grey, or even olive-green, helping to camouflage them against their preferred roosting environments. They are primarily insectivorous, but will also eat a wide range of small vertebrates.</SPAN></SPAN></DIV></div>
HTMLText_6B9D048F_5A02_CCBC_41D0_0AE9A343B57C_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Unidentified cave-dwelling insects. The thread-like lines seen in the picture are sticky webs produced by the larvae to catch food. These webs are similar to the web of glowworms. Glowworm or glow-worm is the common name for various groups of insect larvae and adult larviform females that glow through bioluminescence.</SPAN></SPAN></DIV></div>
HTMLText_6B9D048F_5A02_CCBC_41D0_0AE9A343B57C.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Unidentified cave-dwelling insects. The thread-like lines seen in the picture are sticky webs produced by the larvae to catch food. These webs are similar to the web of glowworms. Glowworm or glow-worm is the common name for various groups of insect larvae and adult larviform females that glow through bioluminescence.</SPAN></SPAN></DIV></div>
HTMLText_7A832817_5A02_43AB_41C8_64F7C3FDB345_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Unidentified species millipedes were found in the cave. They live in complete darkness.</SPAN></SPAN></DIV></div>
HTMLText_7A832817_5A02_43AB_41C8_64F7C3FDB345.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Unidentified species millipedes were found in the cave. They live in complete darkness.</SPAN></SPAN></DIV></div>
HTMLText_441E43D3_5A1E_C4A4_41C3_37134AF54337_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.5vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_441E43D3_5A1E_C4A4_41C3_37134AF54337.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.5vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:1.0012515644555673vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:0.94vw;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_0B4B0DC1_11C0_6277_41A4_201A5BB3F7AE_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:3.9300000000000037vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.93vmin;font-family:'Bebas Neue Bold';">john doe</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.5099999999999985vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:2.51vmin;font-family:'Bebas Neue Bold';">licensed real estate salesperson</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">Tlf.: +11 111 111 111</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">jhondoe@realestate.com</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">www.loremipsum.com</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.529999999999997vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.53vmin;">Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.</SPAN></SPAN></DIV></div>
HTMLText_0B4B0DC1_11C0_6277_41A4_201A5BB3F7AE.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:3.9300000000000037vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.93vmin;font-family:'Bebas Neue Bold';">john doe</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.5099999999999985vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:2.51vmin;font-family:'Bebas Neue Bold';">licensed real estate salesperson</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">Tlf.: +11 111 111 111</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">jhondoe@realestate.com</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:2.1899999999999973vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#999999;font-size:2.19vmin;font-family:'Bebas Neue Bold';">www.loremipsum.com</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.42vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;font-size:1.529999999999997vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.53vmin;">Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.</SPAN></SPAN></DIV></div>
HTMLText_6B9CD491_5A02_CCA4_41C7_5E84C47E62D7_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_6B9CD491_5A02_CCA4_41C7_5E84C47E62D7.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_B0E61437_AC1D_D1A5_41E3_C58BFB4DC856_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_453BA95A_5A02_45A4_41C2_02CC6EFE2245.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_440073D5_5A1E_C4AC_41D2_849603713328_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_7A80181A_5A02_43A5_41D4_B6E721A5A388.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_453BA95A_5A02_45A4_41C2_02CC6EFE2245_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_440073D5_5A1E_C4AC_41D2_849603713328.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_443A1854_5A02_43AC_41D3_BEBF0AFC2ED3.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_7A80181A_5A02_43A5_41D4_B6E721A5A388_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_B0E61437_AC1D_D1A5_41E3_C58BFB4DC856.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_443A1854_5A02_43AC_41D3_BEBF0AFC2ED3_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_686A3775_4FA5_659B_41BB_82F140ECD73D.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.6393442622950816vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.6393442622950816vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_686A3775_4FA5_659B_41BB_82F140ECD73D_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628445vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.6393442622950816vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.6393442622950816vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_686B5779_4FA5_658B_41D3_A7F30DBD167C_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_5133F7EB_4FE7_648E_41CD_E1D2CDE1D7BE.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_5133F7EB_4FE7_648E_41CD_E1D2CDE1D7BE_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_510CE5FA_4FE6_A489_41A3_DBE102C27137_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_686B5779_4FA5_658B_41D3_A7F30DBD167C.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_510CE5FA_4FE6_A489_41A3_DBE102C27137.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian age 360 ​​- 245 million years ago, Khlong Min Formation of Jurassic period age 210-140 million years ago, and Lam Thap Formation of Cretaceous age 140-66.5 million years ago, and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.53vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.5300546448087435vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.53vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian period (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as  isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_4402B3DA_5A1E_C4A4_41B8_7B1AAEC0548E.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_04DC47E1_107A_39D9_41A7_BA33892C5C05.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_510F15F7_4FE6_A487_41C7_7D02D0334626.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_B0E54433_AC1D_D1BD_41DD_B004585C2728_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_510F15F7_4FE6_A487_41C7_7D02D0334626_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_443D0858_5A02_43A4_41B4_2488AC4CD2C9_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_7B7EF81F_5A02_43DB_41B5_28C8398C3B75.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_513067E8_4FE7_648A_41C2_EBB31DC0BC57_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_453BA960_5A02_4464_41C1_AAF0DBEBE34F.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_6B9C6495_5A02_CCAC_41D4_1FCFC6F079F8_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_6B9C6495_5A02_CCAC_41D4_1FCFC6F079F8.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_443D0858_5A02_43A4_41B4_2488AC4CD2C9.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_B0E54433_AC1D_D1BD_41DD_B004585C2728.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_7B7EF81F_5A02_43DB_41B5_28C8398C3B75_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_04DC47E1_107A_39D9_41A7_BA33892C5C05_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_4402B3DA_5A1E_C4A4_41B8_7B1AAEC0548E_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_513067E8_4FE7_648A_41C2_EBB31DC0BC57.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_453BA960_5A02_4464_41C1_AAF0DBEBE34F_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area between Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian period, or about 360 million years up to the present sediment. The rock hierarchy from oldest to softest is Kaeng Krachan group of Carboniferous-Permian age 360 ​​- 245 million years old, Klong Min rock group of Ju Rae period. Szik, 210-140 million years old, and Lam Thap stone category. Cretaceous, 140-66.5 million years old, and the present sedimentary group</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area's limestone is in the Ratchaburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. which has a category of carbonate rocks of the Middle to Late Permian period is a distinctive feature Distributed in the southern and lower central regions of Thailand. where many fossils are often found in shallow seas The area consists of limestone, dolomite limestone, dolomite, ranging in size from thin to unlisted. There are ancient tea, corals, algae and persimmons. The Middle to Late Permian period (Murgabian) is about 270-250 million years. and was covered by Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs. For example, in the west in Phang Nga Province, it continues into Phang Nga Bay. Limestone often has cast terrain. forming the shape of a beautiful landscape as well as being a tourist attraction in many beautiful caves It is also an important source of raw materials in the industry.</SPAN></SPAN></DIV></div>
HTMLText_510E35F1_4FE6_A49B_41C8_95E200CF8208.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area of Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian (360 ​​- 245 million years ago), Khlong Min Formation of Jurassic (210-140 million years ago), and Lam Thap Formation of Cretaceous (140-66.5 million years ago), and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The limestone in this area is in Ratburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone, and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs, for example in the west of Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of materials in the industry.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p></div>
HTMLText_512D27E3_4FE7_64BE_41B0_B54C3056D925_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area of Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian (360 ​​- 245 million years ago), Khlong Min Formation of Jurassic (210-140 million years ago), and Lam Thap Formation of Cretaceous (140-66.5 million years ago), and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The limestone in this area is in Ratburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone, and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs, for example in the west of Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of materials in the industry.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p></div>
HTMLText_510E35F1_4FE6_A49B_41C8_95E200CF8208_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area of Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian (360 ​​- 245 million years ago), Khlong Min Formation of Jurassic (210-140 million years ago), and Lam Thap Formation of Cretaceous (140-66.5 million years ago), and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The limestone in this area is in Ratburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone, and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs, for example in the west of Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of materials in the industry.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p></div>
HTMLText_512D27E3_4FE7_64BE_41B0_B54C3056D925.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:left;font-size:6.010928961748616vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">K</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">LANG </SPAN><SPAN STYLE="color:#04a3e1;font-size:6.01vmin;font-family:'Bebas Neue Bold';">C</SPAN><SPAN STYLE="font-size:6.01vmin;font-family:'Bebas Neue Bold';">AVE</SPAN></SPAN></DIV><DIV STYLE="text-align:left;font-size:3.4972677595628463vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">______________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.19vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The area of Ban Khlong Ya and Phang Nga Province is supported by sedimentary and igneous rocks dating from the Carboniferous-Permian, or about 360 million years ago up to the present sediment. The stratigraphy from oldest to youngest is Kaeng Krachan Group of Carboniferous-Permian (360 ​​- 245 million years ago), Khlong Min Formation of Jurassic (210-140 million years ago), and Lam Thap Formation of Cretaceous (140-66.5 million years ago), and the present sedimentary group.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:justify;font-size:1.639344262295083vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">The limestone in this area is in Ratburi Group (Ratburi Group-Prb), which is the name used to refer to the Permian sedimentary rock group. There is a formation of carbonate rocks of the Middle to Late Permian period, which is a prominent feature distributed in the southern and lower central parts of Thailand, where many shallow sea fossils are often found. The area consists of limestone, dolomitic limestone, and dolomite. The fossils found include corals, algae, and persimmons of the Middle to Late Permian (Murgabian), approximately 270-250 million years ago. These carbonate rocks have a karst landscape and are found as isolated hills on the plains and covered with Quaternary sediments. Limestone often forms high mountain ranges with long fault cliffs, for example in the west of Phang Nga Province, it continues into Phang Nga Bay. Limestone often has a karst landscape that forms a beautiful landscape and is home to many beautiful cave-type attractions. It is also an important source of materials in the industry.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:1.64vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p></div>
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HTMLText_38188E66_6C6B_8B72_41D2_7C0DDF458FE1_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 0px 2px rgba(0,0,0,0.6);text-align:center;font-size:1.8579234972677583vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.86vmin;font-family:'Montserrat';"><B>Click the</B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.86vmin;font-family:'Montserrat';"><B> Photo</B></SPAN><SPAN STYLE="font-size:1.86vmin;font-family:'Montserrat';"><B> to see </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.86vmin;font-family:'Montserrat';"><B>PDF</B></SPAN></SPAN></DIV></div>
HTMLText_51F45695_7946_F575_41B1_79A721DA8208_mobile.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:1.87vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:2.9850746268656696vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.99vw;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:2.99vw;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.99vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:2.99vw;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.37vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:1.865671641791049vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:1.87vw;font-family:'Montserrat';"><B>G</B></SPAN><SPAN STYLE="font-size:1.87vw;font-family:'Montserrat';"><B>eological </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.87vw;font-family:'Montserrat';"><B>B</B></SPAN><SPAN STYLE="font-size:1.87vw;font-family:'Montserrat';"><B>ackground</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:1.9900497512437707vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.99vw;font-family:'Bebas Neue Bold';">________________________</SPAN></SPAN></DIV></div>
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HTMLText_23F067B8_0C0A_629D_41A9_1A1C797BB055_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>I</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>ntroduction</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:3.497267759562821vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">____________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.4vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Welcome to a virtual tour of Klang cave in Ao Luek District, Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand, and are well-known across Southeast Asia. This cave is around 1 km deep. There are 13 chambers and numerous types of speleothems.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.75vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This virtual tour is designed to allow visitors to view the cave's inside from the comfort of their own homes.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.75vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">In this virtual tour If you press the red hotspot In the panorama, a quiz will appear on the screen. You can select multiple choices in the quiz. If you select the correct answer you will get 1 point, but if you select the wrong answer you will lose 1 point per each answer you select. </SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_7A838815_5A02_43AF_41B3_30790C2FB4A2_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; 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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 0px 3px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_A0E2A3DB_B697_9A20_41C3_A6D60FDBB9EE_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>All stalactites, whatever their composition, begin as hollow soda straws. Initially, a water droplet collects on the cave ceiling due to condensation or water entering through a fracture in the bedrock. With the loss of carbon dioxide, a thin film of carbonate material precipitates and coats the drop's surface. The drop begins to oscillate as it accumulates more water and becomes heavier. This causes the material film to move upward and adhere to the ceiling due to surface tension. When the drop falls, the film remains on the ceiling as a round rim of material; it is the initial growth ring of a soda straw. As drop after drop follows a similar path, an infinitesimal trace of material is left behind, and a hollow tube is formed and eventually enlarged as long as </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>water drips.</B></SPAN></SPAN></DIV></div>
HTMLText_A0022CA2_BDFE_8F5F_41DB_F439714C76F7_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Cave pearls are usually spherical but they can be cylindrical, irregular, cubical, or even hexagonal in shape. They can be as small as a sand grain or as large as eight inches (20 cm) in diameter. Cave pearls are polished and glossy when exposed to moving water; when exposed to air, cave pearls degrade and appear rough. Cave pearls are typically found in shallow cave pools with water dripping in from above or slowly flowing into the pool. Carbon dioxide is lost to the air, carbonate material precipitates around clastic particles in the pool, and excess precipitate material coats the floor and builds up into cups or nests around the pearls. Sand grains, bat bones, shell and wood fragments, or soda straw fragments may serve as nuclei for cave-pearl formation.</B></SPAN></SPAN></DIV></div>
HTMLText_A3730944_B69B_9620_41C7_C5EEAB9CEE3C_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Cave popcorn, or coralloids, are made of calcite, gypsum, or aragonite deposits. These cave stones are small in shape. Most are about a few millimeters to a centimeter in size. Cave popcorn can form by precipitation. Water seeping through limestone walls or splashing onto them leaves deposits when carbon dioxide loss causes its minerals to precipitate. When formed in this manner, the resulting nodules resemble small flowstone balls. Cave popcorn can also form through evaporation in which case it is chalky and white, similar to edible popcorn.  They can grow from cave walls or grow from other cave rocks. Some species consist entirely of calcite and accumulate wasps along cave walls and flow down waterways or along the sides of stalagmites.</B></SPAN></SPAN></DIV></div>
HTMLText_A1B8DEE5_B69B_6BE0_41E0_14EDC4437158_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Columns are neither stalactites nor stalagmites; they are both, together. When a stalagmite grows alongside its feeder stalactite, a new speleothem known as a column or pillar is formed. Columns can grow to enormous proportions, sometimes exceeding 20 meters in height and diameter. The largest columns are typically aligned along ceiling joints, where the most water is dripping into the cave.</B></SPAN></SPAN></DIV></div>
HTMLText_A1B13500_B695_BE21_41D2_35632D019251_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Flowstones are formed by a thin layer of precipitation that sometimes develops into a more rounded shape as it thickens. Flowstone forms where water flows down the walls or along the floors of a cave. The slab-like deposition that protrudes from the wall may be called Curtain or Drapery, sometimes translucent and partially with brown and beige banding with a bacon-like appearance, sometimes called cave bacon. Flowstones are among the largest of speleothems. However, flowstones can be damaged with a single touch. This is due to changes in the crystallization equilibrium of the mineral caused by changes in temperature and oil from human hands. Flowstone is a good indicator of drought because it is caused by runoff buildup; a prolonged lack of water will leave traces of a lack of deposition in the rock and structure details.</B></SPAN></SPAN></DIV></div>
HTMLText_A0140110_B69D_9620_41D7_6C1C8D77399B_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Frostwork is a type of speleothem with needle-like growths. Most frostwork has a spiny appearance due to the acicular habit of aragonite. Frostwork, on the other hand, can be made of calcite, opal, gypsum, other minerals, and ice. Frostwork can be found on cave popcorn, boxwork , stalactites, walls, ceilings, and even floors on rare occasions. The origins of frostwork are somewhat debatable. Cave frostwork is thought to have formed as a result of moist, circulating air containing dissolved calcium carbonate that drifted against rock surfaces and coated them with delicate crystals. Frostwork has also been attributed to water seepage from cave passageways where evaporation rates are relatively high.</B></SPAN></SPAN></DIV></div>
HTMLText_A0314CEF_B675_AFE0_41E4_6C8AB5930FCB_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Speleothems are formed by water. Rainwater percolates through the soil, absorbing carbon dioxide gas and producing weak carbonic acid. This weak acid passes through limestone joints and cracks. </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The mineral calcite dissolves from the limestone rock that forms a cave. When this water, which contains the dissolved rock, is exposed to the cave air, it releases carbon dioxide into the cave atmosphere, causing the water to precipitate calcite in various forms of speleothems. Calcite precipitates on ceilings are called Stalactites. On floors, they are called Stalagmites.</B></SPAN></SPAN></DIV></div>
HTMLText_A0C1120D_B695_9A20_41AD_557A94813288_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Stalagmites are convex floor deposits formed by water dripping from the cave ceiling or from a stalactite overhead. Because falling water droplets tend to splash, stalagmites spread out as they gradually build up from the floor. As a result, unlike stalactites, they lack central, hollow tubes. Stalagmites are typically larger in diameter than stalactites above them, and they have rounded tops rather than </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>pointed tips.</B></SPAN></SPAN></DIV></div>
HTMLText_DA36648A_E8A0_0C8B_41E5_C747305B682D_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The cave map can be toggled on and off by clicking on the map icon at the top right of your screen. You can click on red and green spots on the map to change the panorama. Green spots mean panorama with audio narration and red spots mean panorama without audio narration.</B></SPAN></SPAN></DIV></div>
HTMLText_A0E96915_B694_B620_41D5_5C64335E5BC5_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The chamber in front of you connects to the other entrance called Lake Entrance. This chamber has a Buddha image on a platform above water and you can see someone on the platform coming to worship the Buddha image. If you look on the right side, there is a hidden path that you can go to another chamber but it is very dangerous because you need diving equipment to dive to the next room.</B></SPAN></SPAN></DIV></div>
HTMLText_A084A18F_B6B5_9620_41E3_453D4BA336AA_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>This chamber is large and contains lots of speleothems, and the pathways are unclear. It is easy to get lost in this area if you don't have enough flashlights and no one who knows the path within the cave to lead you.</B></SPAN></SPAN></DIV></div>
HTMLText_A09E1962_B695_96E0_41D0_A60D19636F7F_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are almost at the other entrance which is connected to the next chamber. This chamber contains Buddha images that are worshiped by monks, villagers, and tourists. If you look down, you'll see that you're walking in the water and you'll have to wade through the water to reach the next chamber.</B></SPAN></SPAN></DIV></div>
HTMLText_A0D7B970_B6AB_96E0_41DD_1B6F276250EA_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in a chamber near the cave's end. There are very few speleothems in this chamber. However, it is filled with large amounts of sediment and rockfall. The area is also steep, making walking dangerous because sediments and rockfalls on the floor have the potential to slide and collapse.</B></SPAN></SPAN></DIV></div>
HTMLText_A0E27674_B6B4_9AE1_41D1_0AC3B6CF78FD_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the Emerald Pool Chamber. This chamber is called Emerald pool because it has a large pool of water whose color looks like an emerald when light is reflected by the water. Moreover, this chamber still has columns, flowstones, cave popcorns,  stalagmites, and stalactites.</B></SPAN></SPAN></DIV></div>
HTMLText_A3265762_B6BB_7AE0_41D2_4C30A96E28A7_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the Great Wall Chamber, and in front of you are speleothems known as Rimstone dams. Rimstone dams are a form of speleothems that form where there is some gradient and hence flow, over the edge of a pool. The turbulence caused by flow over the edge of the building dam may contribute to the outgassing from water, causing the crystallization of minerals on the edge of the pool to form the edge of the dam. If there is a large amount of water, Rimstone dams tend to rise with steep slopes. If the amount of water is low, the dam will be shallow. The slope will decrease accordingly.</B></SPAN></SPAN></DIV></div>
HTMLText_A0471DA4_B674_EE61_4184_656A7214DA50_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You've arrived at the Coffee Straws Chamber. This chamber is known as the coffee straws chamber because it contains a type of speleothem that resembles coffee straws known as soda straws. Soda straws, or simply straws, are among the most delicate speleothems. The slightest touch can easily crush or break them. As a result, soda straws are rarely found within arm's reach in show caves or other places with unrestricted access.</B></SPAN></SPAN></DIV></div>
HTMLText_A0A3A08A_BDFE_776E_41E7_51B64C7A1419_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Helictites are twisted speleothems that twist in every direction, making it seem like they were grown in zero gravity. Helictites are among the most fragile cave formations. They are usually made of needle-form calcite and aragonite. Helictite forms have been described in several types such as saws, threads, butterflies, hands, curly-fries, twigs, antlers, and worms. They are usually symmetrical in the radial direction. </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 1.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The slightest touch can easily crush or break them. As a result, helictites are rarely seen within the arm's reach of tourists in tourist caves. The evolution of helictites is still a mystery. There has never been a satisfactory explanation for how they form. Currently, formation by capillary force is the most likely hypothesis, but wind formation is also viable.</B></SPAN></SPAN></DIV></div>
HTMLText_F406A154_E6C3_5412_41D4_5E6DF0D6DC94_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Carbonate rocks of the Middle to Late Permian period are scattered in the southern and lower central parts of Thailand. The limestone bedrock in Krabi province is part of the Ratburi Group, which is the name used to refer to the Permian age of sedimentary rock. Limestone in this area is characterized by high spiky mountains. This type of topography is called Karst topography. Klang cave has developed in Tower karst, a tower-like limestone mountain near the Khlong Marui Fracture Zone.</B></SPAN></SPAN></DIV></div>
HTMLText_EB192292_E6C1_7417_41B7_CDC7004E71B3_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the first chamber of the cave called the large chamber, which is one of the biggest chambers. At this point, the cave is completely dark. If you turn on the flashlight, you will see many speleothems such as stalactites, stalagmites, columns, and flowstones. You should wear a safety helmet and turn on your flashlight at all times from now on.</B></SPAN></SPAN></DIV></div>
HTMLText_0941984A_0351_7526_41A6_0D219E545DBF_mobile.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:0.75vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.75vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:1.0012515644555644vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:1vw;font-family:'Montserrat';"><B>More options include Score report, Mute/Unmute, Change Language and Fullscreen at bottom right of of your screen.</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.75vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:1.0012515644555644vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:1vw;font-family:'Montserrat';"><B>ตัวเลือกเพิ่มเติม ได้แก่ รายงานคะแนน, ปิด/เปิดเสียง, เปลี่ยนภาษา, เต็มหน้าจอ ที่มุมล่างขวาของจอคุณ</B></SPAN></SPAN></DIV></div>
HTMLText_A11E4DC2_B67B_AE20_41E5_E8A65D963480_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Before you enter the cave, you need to check all equipment needed for your safety such as safety helmet, flashlight, enclosed shoes, gloves, and some instant food and water if you plan to stay a long day in the cave. Caves are extremely vulnerable to changing conditions caused by visitors. Therefore, tourists should avoid behaviors that will cause damage to the cave as follows: do not touch stalagmites, stalactites, or other speleothems, do not write on walls, rocks, or things inside the cave, do not take things out of the cave, and do not leave garbage inside the cave.</B></SPAN></SPAN></DIV></div>
HTMLText_F5ACC712_E6C1_7C16_41B5_1E584DFD0611_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Klang cave was formerly known in Thai as Tham Kang. Kang refers to a species of fish that has frequently been found in the pool in front of the cave and in this cave. In 1987, Mr. Poonsak Khansai and the villagers went to explore the cave and discovered that there were a thousand beautiful stalagmites and stalactites in the cave. They explored pathways inside the cave and found a way that leads to the other side of the mountain. Tham Kang was opened to tourists later on.</B></SPAN></SPAN></DIV></div>
HTMLText_F4D023B5_E6C1_F412_41C1_78BDF75B81C3_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Welcome to a virtual tour of Klang cave in Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand and are well-known across Southeast Asia. This cave is around 1 km long. There are 13 chambers and numerous types of speleothems. Here you are standing in front of the cave entrance. You can move between scenes by clicking a hotspot. You can find details about this virtual tour such as Introduction, Map, Geological Background, etc </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 2.5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>at the menu bar at the bottom of your screen.</B></SPAN></SPAN></DIV></div>
HTMLText_69AD15F0_5A02_4C65_41AE_FD0A275102E3_mobile.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 3px rgba(0,0,0,0.7);text-align:center;font-size:2.1902377972465574vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.19vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:2.19vw;font-family:'Montserrat';"><B>ave </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.19vw;font-family:'Montserrat';"><B>P</B></SPAN><SPAN STYLE="font-size:2.19vw;font-family:'Montserrat';"><B>opcorn</B></SPAN></SPAN></DIV></div>
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HTMLText_E071AAE6_FCA6_8015_41EE_2FED8AE0DBAF_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 3px rgba(51,51,51,0.7);text-align:center;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Hydroclimate variability of central Indo-Pacific region</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 3px rgba(51,51,51,0.7);text-align:center;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>during the Holocene</B></SPAN></SPAN></DIV></div>
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HTMLText_51F45695_7946_F575_41B1_79A721DA8208.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:1.87vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:2.9850746268656696vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.99vw;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:2.99vw;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.99vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:2.99vw;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.37vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.865671641791049vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:1.87vw;font-family:'Montserrat';"><B>G</B></SPAN><SPAN STYLE="font-size:1.87vw;font-family:'Montserrat';"><B>eological </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.87vw;font-family:'Montserrat';"><B>B</B></SPAN><SPAN STYLE="font-size:1.87vw;font-family:'Montserrat';"><B>ackground</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.9900497512437707vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.99vw;font-family:'Bebas Neue Bold';">________________________</SPAN></SPAN></DIV></div>
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HTMLText_51FC3F27_7942_D354_41C6_5ECC70CCE88F.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:2.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:2.690863579474342vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>ave </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>D</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>welling </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>S</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>nake</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354194vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.88vw;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV></div>
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HTMLText_453D0953_5A02_45A4_41D5_934377F0AEF2.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:2.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:2.690863579474342vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>F</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>alse </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>ampire </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>B</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>ats</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354194vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.88vw;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV></div>
HTMLText_4435C850_5A02_43A4_41D0_2CBBE5E575FB.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:2.69vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:2.690863579474342vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>H</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>untsman </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:2.69vw;font-family:'Montserrat';"><B>S</B></SPAN><SPAN STYLE="font-size:2.69vw;font-family:'Montserrat';"><B>piders</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354194vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.88vw;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV></div>
HTMLText_51982246_7942_2DD4_41A4_00EB028E6E42.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.003754693366706vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3vw;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:3vw;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:3vw;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354196vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>irtual </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B>T</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>our</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354194vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.88vw;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV></div>
HTMLText_441E73D3_5A1E_C4A4_41CA_8C9544997D0F.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.003754693366706vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3vw;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:3vw;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3vw;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:3vw;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354196vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>irtual </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B>T</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>our</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354194vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:1.88vw;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV></div>
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HTMLText_23F067B8_0C0A_629D_41A9_1A1C797BB055.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>I</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>ntroduction</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.497267759562821vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.5vmin;font-family:'Bebas Neue Bold';">____________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:2.4vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Welcome to a virtual tour of Klang cave in Ao Luek District, Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand, and are well-known across Southeast Asia. This cave is around 1 km deep. There are 13 chambers and numerous types of speleothems.</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.75vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">This virtual tour is designed to allow visitors to view the cave's inside from the comfort of their own homes.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.75vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:justify;font-size:1.7486338797814245vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">In this virtual tour If you press the red hotspot In the panorama, a quiz will appear on the screen. You can select multiple choices in the quiz. If you select the correct answer you will get 1 point, but if you select the wrong answer you will lose 1 point per each answer you select. </SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_441E33D2_5A1E_C4A4_41D3_0B61F80B6960.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:5.245901639344253vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>lang </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:5.25vmin;font-family:'Montserrat';"><B>C</B></SPAN><SPAN STYLE="font-size:5.25vmin;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>V</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>irtual </B></SPAN><SPAN STYLE="color:#04a3e1;font-size:3.28vmin;font-family:'Montserrat';"><B>T</B></SPAN><SPAN STYLE="font-size:3.28vmin;font-family:'Montserrat';"><B>our</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.2786885245901702vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="font-size:3.28vmin;font-family:'Bebas Neue Bold';">_________________________</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.09vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><p STYLE="margin:0; line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; 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white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
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line-height:0.98vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Creative and Research Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.87vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Wonlop Panityayon </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Associate Prof. Dr. Sakonvan Chawchai</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Sukonmeth Jitmahantakul</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Assistant Prof. Dr. Raphael Bissen</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Department of Geology, Faculty of Science, </SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Chulalongkorn University</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:1.2vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';"><B>Field Support Team</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Niwat Wathanayomnaporn</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Manatthawut ChuSaeng</SPAN></SPAN></DIV><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814194vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.64vmin;font-family:'Montserrat';">  •  </SPAN><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Tasnai Sukkeewan</SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.66vmin;"><BR STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-size:0.77vmin;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:1px 1px 6px rgba(0,0,0,0.7);text-align:left;font-size:1.7486338797814232vmin;"><SPAN STYLE="display:inline-block; letter-spacing:0vmin; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1.75vmin;font-family:'Montserrat';">Krabi Caving Club</SPAN></SPAN></DIV></div>
HTMLText_A0E2A3DB_B697_9A20_41C3_A6D60FDBB9EE.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>All stalactites, whatever their composition, begin as hollow soda straws. Initially, a water droplet collects on the cave ceiling due to condensation or water entering through a fracture in the bedrock. With the loss of carbon dioxide, a thin film of carbonate material precipitates and coats the drop's surface. The drop begins to oscillate as it accumulates more water and becomes heavier. This causes the material film to move upward and adhere to the ceiling due to surface tension. When the drop falls, the film remains on the ceiling as a round rim of material; it is the initial growth ring of a soda straw. As drop after drop follows a similar path, an infinitesimal trace of material is left behind, and a hollow tube is formed and eventually enlarged as long as </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>water drips.</B></SPAN></SPAN></DIV></div>
HTMLText_A0022CA2_BDFE_8F5F_41DB_F439714C76F7.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Cave pearls are usually spherical but they can be cylindrical, irregular, cubical, or even hexagonal in shape. They can be as small as a sand grain or as large as eight inches (20 cm) in diameter. Cave pearls are polished and glossy when exposed to moving water; when exposed to air, cave pearls degrade and appear rough. Cave pearls are typically found in shallow cave pools with water dripping in from above or slowly flowing into the pool. Carbon dioxide is lost to the air, carbonate material precipitates around clastic particles in the pool, and excess precipitate material coats the floor and builds up into cups or nests around the pearls. Sand grains, bat bones, shell and wood fragments, or soda straw fragments may serve as nuclei for cave-pearl formation.</B></SPAN></SPAN></DIV></div>
HTMLText_A3730944_B69B_9620_41C7_C5EEAB9CEE3C.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Cave popcorn, or coralloids, are made of calcite, gypsum, or aragonite deposits. These cave stones are small in shape. Most are about a few millimeters to a centimeter in size. Cave popcorn can form by precipitation. Water seeping through limestone walls or splashing onto them leaves deposits when carbon dioxide loss causes its minerals to precipitate. When formed in this manner, the resulting nodules resemble small flowstone balls. Cave popcorn can also form through evaporation in which case it is chalky and white, similar to edible popcorn.  They can grow from cave walls or grow from other cave rocks. Some species consist entirely of calcite and accumulate wasps along cave walls and flow down waterways or along the sides of stalagmites.</B></SPAN></SPAN></DIV></div>
HTMLText_A1B8DEE5_B69B_6BE0_41E0_14EDC4437158.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Columns are neither stalactites nor stalagmites; they are both, together. When a stalagmite grows alongside its feeder stalactite, a new speleothem known as a column or pillar is formed. Columns can grow to enormous proportions, sometimes exceeding 20 meters in height and diameter. The largest columns are typically aligned along ceiling joints, where the most water is dripping into the cave.</B></SPAN></SPAN></DIV></div>
HTMLText_A1B13500_B695_BE21_41D2_35632D019251.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Flowstones are formed by a thin layer of precipitation that sometimes develops into a more rounded shape as it thickens. Flowstone forms where water flows down the walls or along the floors of a cave. The slab-like deposition that protrudes from the wall may be called Curtain or Drapery, sometimes translucent and partially with brown and beige banding with a bacon-like appearance, sometimes called cave bacon. Flowstones are among the largest of speleothems. However, flowstones can be damaged with a single touch. This is due to changes in the crystallization equilibrium of the mineral caused by changes in temperature and oil from human hands. Flowstone is a good indicator of drought because it is caused by runoff buildup; a prolonged lack of water will leave traces of a lack of deposition in the rock and structure details.</B></SPAN></SPAN></DIV></div>
HTMLText_A0140110_B69D_9620_41D7_6C1C8D77399B.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Frostwork is a type of speleothem with needle-like growths. Most frostwork has a spiny appearance due to the acicular habit of aragonite. Frostwork, on the other hand, can be made of calcite, opal, gypsum, other minerals, and ice. Frostwork can be found on cave popcorn, boxwork , stalactites, walls, ceilings, and even floors on rare occasions. The origins of frostwork are somewhat debatable. Cave frostwork is thought to have formed as a result of moist, circulating air containing dissolved calcium carbonate that drifted against rock surfaces and coated them with delicate crystals. Frostwork has also been attributed to water seepage from cave passageways where evaporation rates are relatively high.</B></SPAN></SPAN></DIV></div>
HTMLText_A0314CEF_B675_AFE0_41E4_6C8AB5930FCB.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Speleothems are formed by water. Rainwater percolates through the soil, absorbing carbon dioxide gas and producing weak carbonic acid. This weak acid passes through limestone joints and cracks. </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The mineral calcite dissolves from the limestone rock that forms a cave. When this water, which contains the dissolved rock, is exposed to the cave air, it releases carbon dioxide into the cave atmosphere, causing the water to precipitate calcite in various forms of speleothems. Calcite precipitates on ceilings are called Stalactites. On floors, they are called Stalagmites.</B></SPAN></SPAN></DIV></div>
HTMLText_A0C1120D_B695_9A20_41AD_557A94813288.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Stalagmites are convex floor deposits formed by water dripping from the cave ceiling or from a stalactite overhead. Because falling water droplets tend to splash, stalagmites spread out as they gradually build up from the floor. As a result, unlike stalactites, they lack central, hollow tubes. Stalagmites are typically larger in diameter than stalactites above them, and they have rounded tops rather than </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>pointed tips.</B></SPAN></SPAN></DIV></div>
HTMLText_DA36648A_E8A0_0C8B_41E5_C747305B682D.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The cave map can be toggled on and off by clicking on the map icon at the top right of your screen. You can click on red and green spots on the map to change the panorama. Green spots mean panorama with audio narration and red spots mean panorama without audio narration.</B></SPAN></SPAN></DIV></div>
HTMLText_A0E96915_B694_B620_41D5_5C64335E5BC5.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The chamber in front of you connects to the other entrance called Lake Entrance. This chamber has a Buddha image on a platform above water and you can see someone on the platform coming to worship the Buddha image. If you look on the right side, there is a hidden path that you can go to another chamber but it is very dangerous because you need diving equipment to dive to the next room.</B></SPAN></SPAN></DIV></div>
HTMLText_A084A18F_B6B5_9620_41E3_453D4BA336AA.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>This chamber is large and contains lots of speleothems, and the pathways are unclear. It is easy to get lost in this area if you don't have enough flashlights and no one who knows the path within the cave to lead you.</B></SPAN></SPAN></DIV></div>
HTMLText_A09E1962_B695_96E0_41D0_A60D19636F7F.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are almost at the other entrance which is connected to the next chamber. This chamber contains Buddha images that are worshiped by monks, villagers, and tourists. If you look down, you'll see that you're walking in the water and you'll have to wade through the water to reach the next chamber.</B></SPAN></SPAN></DIV></div>
HTMLText_A0D7B970_B6AB_96E0_41DD_1B6F276250EA.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in a chamber near the cave's end. There are very few speleothems in this chamber. However, it is filled with large amounts of sediment and rockfall. The area is also steep, making walking dangerous because sediments and rockfalls on the floor have the potential to slide and collapse.</B></SPAN></SPAN></DIV></div>
HTMLText_A0E27674_B6B4_9AE1_41D1_0AC3B6CF78FD.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the Emerald Pool Chamber. This chamber is called Emerald pool because it has a large pool of water whose color looks like an emerald when light is reflected by the water. Moreover, this chamber still has columns, flowstones, cave popcorns,  stalagmites, and stalactites.</B></SPAN></SPAN></DIV></div>
HTMLText_A3265762_B6BB_7AE0_41D2_4C30A96E28A7.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the Great Wall Chamber, and in front of you are speleothems known as Rimstone dams. Rimstone dams are a form of speleothems that form where there is some gradient and hence flow, over the edge of a pool. The turbulence caused by flow over the edge of the building dam may contribute to the outgassing from water, causing the crystallization of minerals on the edge of the pool to form the edge of the dam. If there is a large amount of water, Rimstone dams tend to rise with steep slopes. If the amount of water is low, the dam will be shallow. The slope will decrease accordingly.</B></SPAN></SPAN></DIV></div>
HTMLText_A0471DA4_B674_EE61_4184_656A7214DA50.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You've arrived at the Coffee Straws Chamber. This chamber is known as the coffee straws chamber because it contains a type of speleothem that resembles coffee straws known as soda straws. Soda straws, or simply straws, are among the most delicate speleothems. The slightest touch can easily crush or break them. As a result, soda straws are rarely found within arm's reach in show caves or other places with unrestricted access.</B></SPAN></SPAN></DIV></div>
HTMLText_94357EBC_AA67_2EE5_41C6_DC02CFE99982.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#ffffff;font-size:0.94vw;font-family:'Montserrat';"><B>Click on the circle to start.</B></SPAN></SPAN></DIV></div>
HTMLText_A0A3A08A_BDFE_776E_41E7_51B64C7A1419.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Helictites are twisted speleothems that twist in every direction, making it seem like they were grown in zero gravity. Helictites are among the most fragile cave formations. They are usually made of needle-form calcite and aragonite. Helictite forms have been described in several types such as saws, threads, butterflies, hands, curly-fries, twigs, antlers, and worms. They are usually symmetrical in the radial direction. </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 3px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>The slightest touch can easily crush or break them. As a result, helictites are rarely seen within the arm's reach of tourists in tourist caves. The evolution of helictites is still a mystery. There has never been a satisfactory explanation for how they form. Currently, formation by capillary force is the most likely hypothesis, but wind formation is also viable.</B></SPAN></SPAN></DIV></div>
HTMLText_F406A154_E6C3_5412_41D4_5E6DF0D6DC94.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Carbonate rocks of the Middle to Late Permian period are scattered in the southern and lower central parts of Thailand. The limestone bedrock in Krabi province is part of the Ratburi Group, which is the name used to refer to the Permian age of sedimentary rock. Limestone in this area is characterized by high spiky mountains. This type of topography is called Karst topography. Klang cave has developed in Tower karst, a tower-like limestone mountain near the Khlong Marui Fracture Zone.</B></SPAN></SPAN></DIV></div>
HTMLText_EB192292_E6C1_7417_41B7_CDC7004E71B3.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>You are standing in the first chamber of the cave called the large chamber, which is one of the biggest chambers. At this point, the cave is completely dark. If you turn on the flashlight, you will see many speleothems such as stalactites, stalagmites, columns, and flowstones. You should wear a safety helmet and turn on your flashlight at all times from now on.</B></SPAN></SPAN></DIV></div>
HTMLText_0941984A_0351_7526_41A6_0D219E545DBF.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:0.75vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.75vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:1.0012515644555644vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:1vw;font-family:'Montserrat';"><B>More options include Score report, Mute/Unmute, Change Language and Fullscreen at bottom right of of your screen.</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.75vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:1.0012515644555644vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:1vw;font-family:'Montserrat';"><B>ตัวเลือกเพิ่มเติม ได้แก่ รายงานคะแนน, ปิด/เปิดเสียง, เปลี่ยนภาษา, เต็มหน้าจอ ที่มุมล่างขวาของจอคุณ</B></SPAN></SPAN></DIV></div>
HTMLText_A11E4DC2_B67B_AE20_41E5_E8A65D963480.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Before you enter the cave, you need to check all equipment needed for your safety such as safety helmet, flashlight, enclosed shoes, gloves, and some instant food and water if you plan to stay a long day in the cave. Caves are extremely vulnerable to changing conditions caused by visitors. Therefore, tourists should avoid behaviors that will cause damage to the cave as follows: do not touch stalagmites, stalactites, or other speleothems, do not write on walls, rocks, or things inside the cave, do not take things out of the cave, and do not leave garbage inside the cave.</B></SPAN></SPAN></DIV></div>
HTMLText_F5ACC712_E6C1_7C16_41B5_1E584DFD0611.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Klang cave was formerly known in Thai as Tham Kang. Kang refers to a species of fish that has frequently been found in the pool in front of the cave and in this cave. In 1987, Mr. Poonsak Khansai and the villagers went to explore the cave and discovered that there were a thousand beautiful stalagmites and stalactites in the cave. They explored pathways inside the cave and found a way that leads to the other side of the mountain. Tham Kang was opened to tourists later on.</B></SPAN></SPAN></DIV></div>
HTMLText_F4D023B5_E6C1_F412_41C1_78BDF75B81C3.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>Welcome to a virtual tour of Klang cave in Krabi Province, Southern Thailand. The most stunning speleothems of any kind can be found here. Stalactites and stalagmites at Klang cave are considered the most beautiful in Thailand and are well-known across Southeast Asia. This cave is around 1 km long. There are 13 chambers and numerous types of speleothems. Here you are standing in front of the cave entrance. You can move between scenes by clicking a hotspot. You can find details about this virtual tour such as Introduction, Map, Geological Background, etc </B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 5px rgba(0,0,0,1);line-height:124%;text-align:center;font-size:0.9386733416770964vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#cccccc;font-size:0.94vw;font-family:'Montserrat';"><B>at the menu bar at the bottom of your screen.</B></SPAN></SPAN></DIV></div>
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HTMLText_5194679C_7946_537B_41B9_0B3B7B522AF9.html = <div style="text-align:left; color:#000; "><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:2px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:3.003754693366706vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:3vw;font-family:'Montserrat';"><B>R</B></SPAN><SPAN STYLE="font-size:3vw;font-family:'Montserrat';"><B>esearch</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.38vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-shadow:2px 1px 6px rgba(0,0,0,0.7);text-align:center;font-size:1.877346683354196vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B>K</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>lang</B></SPAN><SPAN STYLE="color:#04a3e1;font-size:1.88vw;font-family:'Montserrat';"><B> C</B></SPAN><SPAN STYLE="font-size:1.88vw;font-family:'Montserrat';"><B>ave</B></SPAN></SPAN></DIV></div>
HTMLText_E071AAE6_FCA6_8015_41EE_2FED8AE0DBAF.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-shadow:2px 1px 6px rgba(51,51,51,0.7);text-align:center;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>Hydroclimate variability of central Indo-Pacific region</B></SPAN></SPAN></DIV><DIV STYLE="text-shadow:2px 1px 6px rgba(51,51,51,0.7);text-align:center;font-size:1.0012515644555693vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;"><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';"><B>during the Holocene</B></SPAN></SPAN></DIV></div>
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HTMLText_519913C6_7946_F2D7_41CB_1CEEB7855DC7.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Klang Cave is formed by the dissolution of Permian limestone within an isolated karst tower in Krabi Province, which is part of the Ratburi Group (orange and brown in the geological map). In this region, most inland karst towers and hills of Jurassic (blue) and Cretaceous (green) sedimentary rocks rise above Quaternary alluvial and colluvial plains forming a series of north-south ridges. Cretaceous granite (pink) is also distributed within this north-south structural trend of the Sibumasu tectonic block.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.93vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;"><B>Further reading</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.37vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.995024875621892vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Geological Map of Changwat Krabi (http://www.dmr.go.th/ download/00user/zoning/</SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';text-indent:17.91px;">แผนที่ธรณีวิทยาจังหวัดกระบี่</SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">.pdf)</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Harper, S. B., Morphology of Tower Karst in Krabi, Southern Thailand. Department of Geology, East Carolina University, Greenville, NC 27858,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Ridd, M.F., Barber, A.J., and Crow, M.J. (Eds), 2011. The Geology of Thailand. Geological Society, London</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Whaley, J., 2021. Geotourism: Thailand - Cliffs, Kayaks and Krabi. GEO ExPro. Vol. 18, No. 4 ( https://www.geoexpro.com/articles/2021/10/geotourism-thailand-cliffs-kayaks-and-krabi)</SPAN></SPAN></DIV></div>
HTMLText_519913C6_7946_F2D7_41CB_1CEEB7855DC7_mobile.html = <div style="text-align:left; color:#000; "><DIV STYLE="text-align:justify;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-line;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Klang Cave is formed by the dissolution of Permian limestone within an isolated karst tower in Krabi Province, which is part of the Ratburi Group (orange and brown in the geological map). In this region, most inland karst towers and hills of Jurassic (blue) and Cretaceous (green) sedimentary rocks rise above Quaternary alluvial and colluvial plains forming a series of north-south ridges. Cretaceous granite (pink) is also distributed within this north-south structural trend of the Sibumasu tectonic block.  </SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.93vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;"><B>Further reading</B></SPAN></SPAN></DIV><p STYLE="margin:0; line-height:0.37vw;"><BR STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-size:0.44vw;font-family:Arial, Helvetica, sans-serif;"/></p><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.995024875621892vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Geological Map of Changwat Krabi (http://www.dmr.go.th/ download/00user/zoning/</SPAN><SPAN STYLE="color:#333333;font-size:1vw;font-family:'Montserrat';text-indent:17.91px;">แผนที่ธรณีวิทยาจังหวัดกระบี่</SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">.pdf)</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Harper, S. B., Morphology of Tower Karst in Krabi, Southern Thailand. Department of Geology, East Carolina University, Greenville, NC 27858,</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Ridd, M.F., Barber, A.J., and Crow, M.J. (Eds), 2011. The Geology of Thailand. Geological Society, London</SPAN></SPAN></DIV><DIV STYLE="text-align:left;text-indent:17.91px;padding-right:17.91px;font-size:0.9328358208955223vw;"><SPAN STYLE="display:inline-block; letter-spacing:0vw; white-space:pre-wrap;color:#000000;font-family:Arial, Helvetica, sans-serif;text-indent:17.91px;"><SPAN STYLE="color:#333333;font-size:0.93vw;text-indent:17.91px;">  •  </SPAN><SPAN STYLE="color:#333333;font-size:0.93vw;font-family:'Montserrat';text-indent:17.91px;">Whaley, J., 2021. Geotourism: Thailand - Cliffs, Kayaks and Krabi. GEO ExPro. Vol. 18, No. 4 ( https://www.geoexpro.com/articles/2021/10/geotourism-thailand-cliffs-kayaks-and-krabi)</SPAN></SPAN></DIV></div>

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IconButton_31C8B5AF_132B_E5F8_419F_F432250FB59D.toolTip = Fullscreen
IconButton_32CB9727_0353_3B6F_41A3_2E4D522D1EE0_mobile.toolTip = Fullscreen
IconButton_31C8B5AF_132B_E5F8_419F_F432250FB59D_mobile.toolTip = Fullscreen
IconButton_0FE5F114_1366_DAA8_41A8_1EBB17D3C8A0.toolTip = Fullscreen
IconButton_32CB9727_0353_3B6F_41A3_2E4D522D1EE0.toolTip = Fullscreen
IconButton_32CA0724_0353_3B61_4198_CB5D9248C5B7.toolTip = Gyroscope
IconButton_32CA0724_0353_3B61_4198_CB5D9248C5B7_mobile.toolTip = Gyroscope
IconButton_32CA5722_0353_3B61_41B1_07F935AF62AE_mobile.toolTip = Hotspot Visibility
IconButton_32CA5722_0353_3B61_41B1_07F935AF62AE.toolTip = Hotspot Visibility
IconButton_32CA0723_0353_3B67_418D_40F330FE867A.toolTip = Mute / Unmute
IconButton_3377A8DC_13E5_EB58_4180_CB1EBFC9F083.toolTip = Mute / Unmute
IconButton_3377A8DC_13E5_EB58_4180_CB1EBFC9F083_mobile.toolTip = Mute / Unmute
IconButton_32CA0723_0353_3B67_418D_40F330FE867A_mobile.toolTip = Mute / Unmute
IconButton_32CD8721_0353_3B63_415D_0391288A7B5A_mobile.toolTip = Report
IconButton_32CD8721_0353_3B63_415D_0391288A7B5A.toolTip = Report
IconButton_31DD7DD3_13EE_E5A8_418B_F7890D002931_mobile.toolTip = Score
IconButton_31DD7DD3_13EE_E5A8_418B_F7890D002931.toolTip = Score
IconButton_32CA8726_0353_3B61_41AC_FF3240AEE23C.toolTip = TH
IconButton_32CA8726_0353_3B61_41AC_FF3240AEE23C_mobile.toolTip = TH
IconButton_32CAC725_0353_3B63_41B0_DEA5249409AF.toolTip = VR
IconButton_32CAC725_0353_3B63_41B0_DEA5249409AF_mobile.toolTip = VR
IconButton_319F6243_13EF_5EA8_41B2_971A409C2A1C_mobile.toolTip = ไทย
IconButton_319F6243_13EF_5EA8_41B2_971A409C2A1C.toolTip = ไทย

## Tour

### Description

### Title
tour.name = Klang Cave