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Periglacial Relief in Velebit Mountain Area

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Author(s): Dražen Perica | Sanja Lozić | Irena Mrak

Journal: Geoadria
ISSN 1331-2294

Volume: 7;
Issue: 1;
Start page: 5;
Date: 2002;
Original page

Keywords: Velebit mountain | periglacial relief | nival modelling | frost processes and forms

ABSTRACT
Although the Velebit is a low mountain situated in the moderate climate zone, there exist periglacial processes in relief modelling in its highest part. The reason for this is interdependance of geological, geomorphological, climatic, vegetational and pedological influences, but also long antropogenic and zoogenic influences. Among periglacial forms the features which originated from the activity of nival and frost processes can be singled out.
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Tango Jona
Tangokurs Rapperswil-Jona