41 KB7745 KB39 KB198520252011Gostinčar, Petraštevilka:35str. 27-43ISSN:0354-0596COBISSID:47813218URN:URN:NBN:SI:doc-8M5GTWJKslZnanstvena založba Filozofske fakulteteDela - Oddelek za geografijo Filozofske fakultete v Ljubljanicontact karstgeomorfologijageomorphologykarstologyKočevski Rogkontaktni kraskras (geologija)krasoslovjeSloveniaSlovenijaKontaktni kras v Kočevskem Rogu in Kočevski Mali gori|On high Dinaric karst plateaus of Kočevski Rog and Kočevska Mala gora, the so-called contact karst is present. Geomorphic processes and landforms of four case study areas of contact karst were researched in detail. Two types of contact karst were recognized: between non-carbonate and carbonate rocks and between different carbonate rocks. In the first case, ponors and blind valleys (active and fossil) were formed and concave forms near the contact are infilled with non-carbonate sediments. On the contact between different carbonate rocks (dolomite and limestone), the forms are similar but less evident, e.g. ponors (active and fossil), ponor steepheads and dry valleysNa dinarskih kraških planotah Kočevskega Roga in Kočevske Male gore se je na kontaktu med kraškim in fluvialnim geomorfnim sistemom oblikoval t.i. kontaktni kras. Preučene so bile geomorfološke oblike in procesi na štirih območjih kontaktnega krasa. Na stiku med nekarbonatnimi in karbonatnimi kamninami so se razvile ponikve, slepe doline (aktivne in fosilne), konkavne oblike v bližini kontakta pa so zapolnjene z nekarbonatnimi sedimenti. Na kontaktu med različnimi karbonatnimi kamninami (dolomiti in apnenci) so reliefne oblike kontaktnega krasa manj jasno izoblikovane, mdr. ponori (aktivni in fosilni), ponorni zatrepi ter suhe dolineTEXTznanstveno časopisjejournalsSlovenian National E-content AggregatorNational and University Library of SloveniaUniverza v Ljubljani, Filozofska fakulteta