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The Krasno polje is located within the Northern Velebit Mountain in the Dinaric Alps, Croatia. It is completely filled with gravel and is inactive in a hydrological sense. We established that slopes above the polje were intensively modified by glacial action during the colder periods of the Pleistocene. Therefore, proglacial fans filled the karst depression, forming a piedmont polje. We assume that the polje was filled by proglacial material over at least two separate glacial events.Krasno polje se nahaja v severnem Velebitu v Dinarskem gorstvu na Hrvaškem. Kraško polje je popolnoma zapolnjeno s prodom in v hidrološkem pogledu neaktivno. Ugotovili smo, da so bila pobočja nad poljem v hladnejših obdobjih pleistocena izrazito preoblikovana z ledeniškim delovanjem. Tako so predledeniški vršaji zapolnili kraško kotanjo pod njimi in oblikovali piedmontski tip kraškega polja. Domnevamo, da je bilo kraško polje zapolnjeno s predledeniškim materialom vsaj v dveh različnih poledenitvenih fazah

Geomorfološke značilnosti Krasnega polja, severni Velebit, Hrvaška