A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2017; you can also visit the original URL.
The file type is
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