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Geomorphological properties of the Krasno polje, Northern Velebit, Croatia
2014
Dela
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.
doi:10.4312/dela.41.5.101-115
fatcat:lcs5eauurbcbdd3ofeunavnuvy