Short History <strong>of</strong> ResearchAndrej Kranjc<strong>Dinaric</strong> karst is <strong>the</strong> landscape where <strong>the</strong>sciences <strong>of</strong> karstology and speleology took<strong>the</strong>ir origin and started to develop thus contributingseveral karstological terms to internationalkarst terminology. In <strong>the</strong> antiquityalready some <strong>of</strong> karst phenomena werementioned <strong>from</strong> <strong>the</strong> <strong>Dinaric</strong> karst, but hereare considered published sources mostly<strong>from</strong> <strong>the</strong> 16 th century on, when <strong>the</strong> modernkarst research started. In those times <strong>Dinaric</strong>karst belonged to different states. Adequatesources were used and and it was a difficulttask yet not completely achieved but it presentsa relatively new approach. For <strong>the</strong> olderperiod some Venetian and Turkish works areincluded. Emphasized are Austrian and Austro-Hungarian researchers working in Bosnia andHerzegovina as well as Serbian researchers.The contribution which can be no more thanan unpretentious overview mentions earlyphilosopher N. Gučetić discussing karst phenomena,and travellers through <strong>the</strong> Balkanslike B. Hacquet, B. Kuripečič, E. Čelebija, andA. Fortis, and also well-known geomorphologistsand speleologists A. Penck, E.-A. Martel,J. Cvijić, A. Melik, and J. Roglić.Pre-scientific phase<strong>Karst</strong> phenomena or better phenomenawhich we are called nowadays as karst onesare relatively <strong>of</strong>ten mentioned by ancientGreek and Roman authors. The groundwaterand its connection with <strong>the</strong> sea are noted byHomer, Thales <strong>of</strong> Millet, Anaxagoras, Plato,Aristotle, Lucretius, and Seneca. Among <strong>the</strong>sedescriptions <strong>the</strong>re are also some <strong>from</strong> <strong>Dinaric</strong>karst. Pseudo-Skylax’s Periplous (The Circumnavigation<strong>of</strong> <strong>the</strong> Inhabited World) <strong>of</strong> 4 th centuryBC mentions <strong>the</strong> springs <strong>of</strong> Timavo (Herak& Stringfield 1974) which were later studiedby Poseidonios <strong>of</strong> Apameia (135 – 50 BC). Inconnection with <strong>the</strong>m he mentions also »<strong>the</strong>chasm« - Škocjanske jame (Škocjan caves;Kranjc 1998). In Virgil’s Aeneida <strong>the</strong> Timavosprings are called <strong>the</strong> Mo<strong>the</strong>r <strong>of</strong> <strong>the</strong> sea andStrabo’s Geography names Lugeon Lacus. Curiouslyall <strong>the</strong>se phenomena are <strong>from</strong> <strong>the</strong> northwesternpart <strong>of</strong> <strong>the</strong> <strong>Dinaric</strong> karst. Taking into<strong>the</strong> consideration that this is <strong>the</strong> most distantrelated to Greece, I would say that we do notknow <strong>the</strong> appropriate references.From <strong>the</strong> Middle Ages it is not knownmuch more. Tabula Peutingeriana showing<strong>the</strong> springs <strong>of</strong> <strong>the</strong> Timavus is in fact a Romanmap. <strong>Karst</strong> phenomena are mentioned in <strong>the</strong>documents <strong>from</strong> different reasons but withouta notion <strong>of</strong> karst yet. In 888 <strong>the</strong> king Berangerdonated <strong>the</strong> church in <strong>the</strong> cave Sv. Ivan vČele – San Giovanni d’Antro located in <strong>the</strong> lastparts <strong>of</strong> <strong>the</strong> karst above <strong>the</strong> plain <strong>of</strong> Friuli, <strong>the</strong>Croatian word for <strong>the</strong> cave Pechice, Pechie orPechine ossia Grotta, that is pećina, figureson <strong>the</strong> map <strong>of</strong> <strong>the</strong> domain <strong>of</strong> a monastery on<strong>the</strong> Ugljan Island in <strong>the</strong> year 1096 and 1166respectively as shown in many contributions<strong>of</strong> late M. Malez (1984). Well known is Byzantine’sEmperor Constantine Porphyrogennetosdescription <strong>of</strong> his empire De AdministrandoImperio (948 – 952) where many karst sites arementioned like <strong>the</strong> rivers Pliva and Buna (one<strong>of</strong> <strong>the</strong> biggest karst springs), poljes <strong>of</strong> Imotskiand Krbava, and <strong>the</strong> place Vrulja (Bury 1920).The study <strong>of</strong> this work <strong>from</strong> <strong>the</strong> karstologicalpoint <strong>of</strong> view is still waiting to be done.It can be said that during <strong>the</strong> 16 th century<strong>the</strong> interest for <strong>the</strong> karst, future karstol-9
ogy started. In 1531 a lawyer <strong>from</strong> Ljubljana,Benedikt Kuripečič (Kuripešič) (born 1490)published a diary <strong>of</strong> his voyage through <strong>the</strong>Balkans as <strong>the</strong> interpreter to <strong>the</strong> Turkish sultanSuleiman to Constantinople (Curipeschitz1531). From <strong>the</strong> point <strong>of</strong> view <strong>of</strong> karst he mentionsjust some karst spring (Kranjc 2008).Equally unimportant is Leonberger’s longpoem about <strong>the</strong> Lake <strong>of</strong> Cerknica. Accordingto <strong>the</strong> description (oral or written) <strong>of</strong> S. Herberstein,Vienna’s diplomat by <strong>the</strong> origin <strong>from</strong>Vipava, G. Wernher (1551) published a description<strong>of</strong> this lake (in fact seasonally floodedpolje), including <strong>the</strong> map (Simoniti 2010). On<strong>the</strong> o<strong>the</strong>r side <strong>of</strong> <strong>Dinaric</strong> karst a philosopher<strong>from</strong> Dubrovnik, Nikola Gučetić (Gozze 1584)published a discussion <strong>of</strong> <strong>the</strong> wind in <strong>the</strong> Cave<strong>of</strong> Vjetrenica (Wind Cave) and <strong>of</strong> <strong>the</strong> speleo<strong>the</strong>ms<strong>from</strong> <strong>the</strong> cave Šipun. The reputation<strong>of</strong> <strong>the</strong> Cerkniško jezero (Cerknica lake) grewwhich can be well seen <strong>from</strong> <strong>the</strong> contemporaneousmaps <strong>of</strong> Lazius, Ortelius or Mercator forexample: <strong>the</strong> lake is drawn much bigger thanit deserves according to <strong>the</strong> scale <strong>of</strong> <strong>the</strong> map.Evliya Çelebi (Evlija Efendi), his full namewas Evlijā ibn Derviš Mehmed Zillī, travelled<strong>the</strong> whole <strong>of</strong> his life (1611 – 1682), a lot throughBalkans too. In his diaries, discovered littlemore than 100 years ago, are described karstlandscapes, water phenomena, caves (mostlyin connection with fighting guerrilla). Curiouslyhe knows a sort <strong>of</strong> corrosion: to make <strong>the</strong>road through limestone terrain large enoughto pass <strong>the</strong> canons, soldiers had to pour <strong>the</strong>acid on <strong>the</strong> limestone (Kranjc 2008)! This isalso a time when one <strong>of</strong> <strong>the</strong> leading scientistsFig. 4: Valvasor’s hydraulic model <strong>of</strong> Cerkniško jezero (Cerknica lake).10
- Page 2 and 3: Andrej Mihevc, Mitja Prelovšek, Na
- Page 4 and 5: ContentsGeographical Position and G
- Page 7: Fig. 2: Coastal part of Dinaric kar
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- Page 13 and 14: GeologyNadja Zupan HajnaThe Dinaric
- Page 15 and 16: ceous. The final disintegration of
- Page 17 and 18: Fig. 11: Locations of Jelar Breccia
- Page 19 and 20: ClimateMitja PrelovšekThe Dinaric
- Page 21 and 22: 311 mm/a; Zaninović 2008) and incr
- Page 23 and 24: 24Fig. 16: Spatial distribution of
- Page 25 and 26: ocks (such as Eocene flysch, Lower
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- Page 29 and 30: GeomorphologyAndrej MihevcIn folk l
- Page 31 and 32: long. They are smoother especially
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- Page 35 and 36: Structural poljes are dominated by
- Page 37 and 38: Fig. 28: Typical dolines of Dinaric
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- Page 43 and 44: Land UseNadja Zupan Hajna, Andrej M
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- Page 47 and 48: Fig. 38: Grančarevo dam in the upp
- Page 49 and 50: KrasThe Kras is a distinct plateau,
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- Page 53 and 54: dolomite barrier along the Idrija w
- Page 55 and 56: of Dolenjska (Gams, 1974; Kranjc, 1
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ly several dozen meters deep. Shaft
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smaller than the higher ones. The r
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tion in the Divaški kras (Mihevc 1
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Use of Karst and its ProtectionThe
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Gams, I., Vrišer, I. (Eds.), 1998:
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lems.- Dela 38, Raziskovalni center