Izvorni znanstveni članak
https://doi.org/10.21861/HGG.2006.68.02.02
Geomorphological Traces of the Younger Pleistocene Glaciation in the Central Part of the Velebit Mt.
Andrija Bognar
; Geografski odsjek, Prirodoslovno-matematički fakultet, Sveučilište u Zagrebu, Zagreb, Hrvatska
Sanja Faivre
orcid.org/0000-0001-7610-1164
; Geografski odsjek, Prirodoslovno-matematički fakultet, Sveučilište u Zagrebu, Zagreb, Hrvatska
Sažetak
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 richess of snow precipitation during the Pleistocene were a very good predisposition for glaciation development on the central part of the Velebit Mt
Ključne riječi
moraines; Pleistocene; glacial valleys; cirques; plateau glaciers; Velebit Mt.; Croatia
Hrčak ID:
20718
URI
Datum izdavanja:
20.12.2006.
Posjeta: 2.729 *