engleski

Geomorphological traces of the younger Pleistocene glaciation in the central part of the Velebit Mt.

On the central part of the Velebit Mountain the traces of the Pleistocene glaciation have been found. The domination of the dissected relief, characterized by numerous elevations and depressions, in the conditions of low temperatures and richness of snow precipitations during Pleistocene were a very good predisposition for the glaciation development on the central part of the Velebit Mt.

moraines; Pleistocene; glacial valleys; cirques; plateau glaciers; Velebit Mt. Croatia

nije evidentirano