20.500.12556/DiRROS-25195 Slovene Classical karst: Kras Plateau and the Recharge Area of Ljubljanica River Klasični kras: planota Kras in kraško zaledje izvirov Ljubljanice The area of the Classical Karst is roughly defined by a triangle with Ljubljana, Trieste and Rijeka as its vertices. This is the area where the first scientific studies of karst phenomena were conducted. Two sub-regions that particularly attracted researchers are presented. Kras/Carso plateau with the Škocjan caves and the underground course of the Reka river. The groundwater flow of Reka-Timavo is characterised by high recharge variability of allogenic inflow of Reka River and flow restrictions in the upper part of subterranean flow, which control regional backfloodings observed in cave systems. The recharge area of Ljubljanica Springs is known for a cascading series of poljes in intermediate cave systems. The area has been in focus of hydrological studies for over a century, but many phenomena have been resolved in the last decade based on results of continuous autonomous monitoring in the last decade. Območje Klasičnega krasa v grobem objema trikotnik z Ljubljano, Reko in Trstom v ogliščih. Tu se je začelo znanstveno proučevanje krasa. Dve kraški območji sta tu še posebej pritegnili pozornost raziskovalcev. Prvo je planota Kras s Škocjanskimi jamami in podzemnim tokom Reke med Škocjanskimi jamami in izviri Timave. Ta tok močno zaznamuje velika spremenljivost dotoka reke Reke in lokalne zožitve v vodonosniku, ki povzročajo regionalno poplavljanje, kot ga beležimo v jamah. Drugo je območje kraške Ljubljanice z značilnim nizom dinarskih kraških polj in jamskih sistemov, ki polja hidrološko povezujejo. Območje je že več kot stoletje predmet številnih raziskav, zvezno spremljanje parametrov toka v kraških jamah v zadnjih desetih letih, pa je omogočilo nova spoznanja o lastnostih in mehanizmih pretakanja vode v celotnem sistemu. Classical Karst Kras Škocjanske Jame Reka-Timavo system Ljubljanica Recharge Area Polje Klasični kras Kras Škocjanske jame podzemni tok reke Reke kraško zaledje izvirov Ljubljanice polje true false true Angleški jezik Slovenski jezik Članek v reviji 2026-01-13 13:56:46 2026-01-13 13:56:46 2026-01-14 03:53:43 0000-00-00 00:00:00 2022 0 0 str. 35-60 št. 2 letn. 63 2022 0000-00-00 Zaloznikova Objavljeno NiDoloceno 0000-00-00 0000-00-00 2022-09-07 556.36:551.4.033(497.4) 1855-7996 10.3986/fbg0097 122774275 https://ojs.sazu.si/folia_bio_geo/article/view/8026 0 556e8968-f080-11f0-94a7-001a4af901a5 https://dirros.openscience.si/Dokument.php?lang=slv&id=37997 _02-geologica_2022_02-gabrovsek_slovene+classical+karst.pdf _02-geologica_2022_02-gabrovsek_slovene+classical+karst.pdf 1 31166B1127D1BA4E90225963F2DF79C4 a1181fa575cd893dc88a52bdac5b0ed26d96692e2a337721d777e7dbb5fd8e09 60992a51-f080-11f0-94a7-001a4af901a5 https://dirros.openscience.si/Dokument.php?lang=slv&id=37998 Slovenska akademija znanosti in umetnosti Folia biologica et geologica 0 0 0