аЯрЁБс>ўџ ;=ўџџџ:џџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџьЅС5@ №П“bjbjЯ2Я2 .­X­Xьџџџџџџˆ€€€€€€€ЖКККК Ц ЖД(оооооЙЙЙ$мR. B59€ЙЙЙЙЙ5€€оолnљљљЙ €о€ољЙљљ€€ов ЕЙ­гКУ  „0Дp Эp ”Ј€€€€Вp €У@ЙЙљЙЙЙЙЙ55ЖЖКуЖЖКUse of GIS and Geological Maps in Speleological Research on the Example of the Northern Part of the Island Cres Nina TRINAJSTI1,2, Velimir IVA I2, Tomislav BANDERA ANI3 1 Public Institution "Priroda", Grivica 4, 51000 Rijeka, Croatia nina.trinajstic@ju-priroda.hr 2 Caving Club Ozren Luki, Drage Gervaisa 23, 10090 Zagreb, Croatia 3 Society for Historical and Cultural Heritage Research "Tramuntana", Beli 4, 51559 Beli, Croatia Abstract Speleology is a set of scientific activities aimed at exploring underground karst phenomena. Underground is one of the most unknown areas on the Earth. Available data are very rare and found in various databases and literature, therefore the preparation of the research is a long-lasting process. Speleological research on the island Cres started with cabinet work, studying literature and reviewing available maps. In the past, classic "paper" maps were used for comparison and research of the area. With development of the GIS this comparison method was significantly improved. GIS has enabled us to convey topographic with geological maps by a simple and fast technique. Why is it important? Some of the relief forms that are characteristic for karst are easily recognized on topographic maps. In addition, a great advantage in finding a possible position of undiscovered speleological objects is given by knowledge of gрю   & ( > L N V X \ ^ ` „ Ъ    6 Ž Ђ Є І ф ц   ( * R f h x | YS]mx‘’“ѓшнбшнбшЦшнбшКЏЦЏшКЏЦЏшКЏЦЄЦ™Џ™ЏшЦЏшЏ—ЏшЏŒЏшшhKeh`eemH sH hKehKemH sH UhKehЫXгmH sH hKeh№2ŸmH sH hKehGUьmH sH hKehцІH*mH sH hKeh№pQmH sH hKehGUьH*mH sH hKehJPŠmH sH hKehцІmH sH hKehцІ5mH sH .ртZ \ о  Ђ f h z | TU‘’“њР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌgdцІ“ўeological structures and lithology. By comparing relief forms and geology, we selected areas with a high probability of finding caves and pits. An exploration of the unknown terrain of the island Cres started with work in GIS, and the results of the previous thorough preparations have led to the discovery of 23 new speleological objects. Keywords: geology, GIS, topographic maps, speleology, karst ,1hАа/ Ар=!А"А# $ %ААФАФ ФœD@ёџD NormalCJ_HaJmH nHsH tHDA@ђџЁD Default Paragraph FontRiѓџГR  Table Normalі4ж l4жaі (kєџС(No List H™@ђH Ke Balloon TextCJOJQJ^JaJьџџџџьpq­Ўя QГДНО­Ўъыю˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€““ “ №8№@ёџџџ€€€ї№’№№0№( № №№B №S №ПЫџ ?№ююЦбюЦбюџџLapaine №"`ž PRЎUЩƒ{Щ'ЬAхbTќž PRКPТгGе гGе ЎUЩ\xЇ#ž PRƒ{Щ'ъd‡rЩ~ 6КPТž PR u]hž PRъd‡rЬAх х щ+-дFG№pQ`eeJPŠKe№2ŸцІЫXгGUьюџ@€ыы„ Йыы4Yь`` `@`0@џџUnknownџџџџџџџџџџџџG‡z €џTimes New Roman5€Symbol3& ‡z €џArial;†SimSun‹[SO5& ‡za€џTahoma"ёˆ№аhп…Xgф™XЧф ф С№ ДДr4dщщ3ƒQ№џ§HP рџ?фџџџџџџџџџџџџџџџџџџџџџщ+-џџ~Title of the presentation:: USE OF GIS AND GEOLOGICAL MAPS IN SPELEOLOGICAL RESEARCH ON THE EXAMPLE OF THE NORTHERN PART OF TLapaineLapaineўџр…ŸђљOhЋ‘+'Гй0$&˜ ,<HX ht  œ ЈДМФЬдфTitle of the presentation:: USE OF GIS AND GEOLOGICAL MAPS IN SPELEOLOGICAL RESEARCH ON THE EXAMPLE OF THE NORTHERN PART OF TitlLapaineapaNormalLapaine3paMicrosoft Word 10.0@Œ†G@8єжг@ џ ­гфGH$џџџџVT$mc •  въ.ћМ"Systemъє|rэЦ0P` ъ-ћœџМ@Times New Roman- ‚2 ДюOьШUse of GIS and Geological Maps in Speleological Research on the Example of the H',2"M'8288M,222,2^28'888,,222+2H,',2,,828!8,C23R8,2"!8,;2 'ю ьШNorthern Part of the Island CresH2,!8,,8<2-!2"!8,''288H,,' 2 'cьШ А6ћœџ@Times New Roman- 2 ˜юьШ А--2 юьШNina TH2,= ћœџю@Times New Roman-.2  ьШRINAJSTIЦD HH(8>C.-№ћНџ@Times New Roman-2 нњьШ1,2""-2 O ьШ, Velimir IG,N! №ћœџю@Times New Roman-.2 №ьШVAШIЦTIHDC.-№- 2 н' ьШ2А"-2 I ьШ, Tomislav =2N',22  ьШBANDERAsBHHH=CH 2 № ьШ А  ћœџю@Times New Roman-.2  ьШANIЦHI C.-№- 2 нў ьШ3А"- 2  ьШ А- 2 ~юьШ А-- 2 УюьШ1А"- 2 ёьШ А&2 ё)ьШPublic Institution822,2'222@2 ём#ьШ "Priroda", Grivica 4, 51000 Rijeka(8!!32,(I!2,,222222C,2,2 ё_ ьШ, CroatiaC!2,, 2 ёЗ ьШ А.%2 dюьШnina.trinajstic@jn22,!2,',\ 2 d‰ьШuА2 2 dЛьШ-А!2 dм ьШpriroda.hr2!!23,2! 2 diьШ А.- 2 ЉюьШ2А"- 2 зьШ А2 з) ьШCaving Club C,221C22з>ћœџю@Times New Roman-.2 з> ьШOzren Lukiц, H-!,2;23,.-№:2 зfьШDrage Gervaisa 23, 10090 ZagrebH!-1,H,!3,',2223222<-2!,22 зГ ьШ, CroatiaiC!3,, 2 з ьШ А.- 2 юьШ3А"- 2 JьШ А:2 J+ьШSociety for Historical and Cult82,,/!2!H'2!-,-22C2 2 JџьШuА2,2 J1ьШral Heritage Research !,H,!-1,C,(,,!,3 2 JБ ьШ"А(2 Jй ьШTramuntana>!,N22,3, 2 JН ьШ"А()2 Jх ьШ, Beli 4, 51559 BeliC,222222B,2 J§ьШ, 2 НюьШCroatiasC!2,, 2 НьШ А- 2 0юьШ А-2 ЃюьШAbstractH2'!,, 2 Ѓ@ьШ А. 2 юьШ А-e2 ‰ю<ьШSpeleology is a set of scientific activities aimed at explor82,,2230',',2!(,,2!,,,2,',N,2,,322!,2 ‰з ьШing underground karst 21222,"1!22223,!'‹2 ќюUьШphenomena. Underground is one of the most unknown areas on the Earth. Available data 22,22N,2,H23,"1!2232'22,2!2,N2'22222H2,!-,'222,=-!2H2,,2,2,,’2 o юZьШare very rare and found in various databases and literature, therefore the preparation of ,!,2-#0!-!,,22!222222,!22'2,,2,(,',22,!,2!,2-!,!3!,2,2",2,!,222!,2 т юьШthe research is a long2,!,'-,!,2',231 2 т 9ьШ-А!A2 т Z$ьШlasting process. Speleological resea,'212!2-,''82,,231,-!,',,:2 т т ьШrch on the island Cres started ",2222,',22D!,'',!,2’2 U юZьШwith cabinet work, studying literature and reviewing available maps. In the past, classic H2,,22,H2!2'24021,!,3!,,22!,2,H21,3,,2,N,2' 23-2,',,'',‰2 Ш юTьШ"paper" maps were used for comparison and research of the area. With development of (2,3,"(N,2'H-!,2',2!2!,2N2,!'22,22!,(,-!,22!2,,!-,_22,2,22N,22!X2 ; ю3ьШthe GIS this comparison method was significantly im2,I82',2N2-!'22N,222H,''12!-,21N82 ; @ ьШproved. GIS has enabled us to 2!22,2I83,',3,2,22'2†2 Ў юRьШconvey topographic with geological maps by a simple and fast technique. Why is it ,222.02231!,22,H21,231-,N,2'40,'O2,,22!,'-,2222,_30'•2 ! ю\ьШimportant? Some of the relief forms that are characteristic for karst are easily recognized N22!,2.82N,2!2,!,,!!2!N'2,-!,,3,!-,,!',!2!3,!',",,,'0!-,312-,2Y2 ” ю4ьШon topographic maps. In addition, a great advantage 222221",22,N,2' 2,2222,1",,,23,2-1,>2 ” "ьШin finding a possible position of 2!2231,22''2,32'222!g2  ю=ьШundiscovered speleological objects is given by knowledge of g222',22,!,2'3,,221-,22,,''12,240223H,22,2!112  Ж ьШeological structures and s,231-,'!3,2!,',22ƒ2 z юPьШlithology. By comparing relief forms and geology, we selected areas with a high 22220D0,2N2-!31!,,!!3!N',221,2330H,',,,,2,",,'H2,212”2 э ю[ьШprobability of finding caves and pits. An exploration of the unknown terrain of the island 2!22,202!!2231--2,',222'H2,322!,222!2,22222H2,!",22!2,',22e2 `ю<ьШCres started with work in GIS, and the results of the previoC!,'',!,2H2H2!23I8,222,!,'2'2!2,2!,2282 `& ьШus thorough preparations have 2'22!23122"-2,!,22'2,2,[2 гю5ьШled to the discovery of 23 new speleological objects.,222,2',22,#02!232,H'2,,231,,22-,' 2 г ьШ А- 2 FюьШ А-2 ЙюьШKeywordsH.0H2!2'#2 ЙˆьШ: geology, GIS, 1,2330J82 Й ьШtopographicG2221!,32,/2 ЙтьШ maps, speleology, karstN,2''2,-22302-!' 2 ЙІ ьШ А- 2 ,юьШ А- 2 ŸюьШ А--ШШььЧЧыыЦЦъъХХщщФФшшУУччТТццССххРРфф П Пу у  О От т  Н Нс с  М Мр р  Л Лп п ККооЙЙннИИммЗЗллЖЖккўџеЭеœ.“—+,љЎ0x hpŒ”œЄ ЌДМФ Ь WфGeodetski fakultet щA Title of the presentation:: USE OF GIS AND GEOLOGICAL MAPS IN SPELEOLOGICAL RESEARCH ON THE EXAMPLE OF THE NORTHERN PART OF T Title ўџџџўџџџўџџџ !"#$%&'()*+,-./01ўџџџ3456789ўџџџ§џџџ<ўџџџўџџџўџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџRoot Entryџџџџџџџџ РF№ўЛ­г>€Data џџџџџџџџџџџџ1TableџџџџWordDocumentџџџџ.SummaryInformation(џџџџџџџџџџџџT&DocumentSummaryInformation8џџџџџџџџ2CompObjџџџџџџџџџџџџjџџџџџџџџџџџџўџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџўџ џџџџ РFMicrosoft Word Document MSWordDocWord.Document.8є9Вq