Abstract
Na 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 doline.
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