Geomorfološke značajke zavale Oštarijskog polja u kršu

The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst proces...

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Veröffentlicht in:	Geoadria 2017-01, Vol.7 (2), p.23-34
Hauptverfasser:	Perica, Dražen, Bognar, Andrija, Lozić, Sanja
Format:	Artikel
Sprache:	hrv ; eng
Schlagworte:	Baške Oštarije karst polje derasion and periglacial processes and relief forms derazijski i periglacijalni procesi i reljefni oblici fluvio-karst fluvio-krški karst krški Oštarijsko polje u kršu Velebit Velebit mountain
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Beschreibung
Zusammenfassung:	The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst processes, the derasion and periglacial processes have been most expressed at the relief formation. The water which flows down from edge parts of polje has great importance in relief formation because of its corrosional aggressivity.
ISSN:	1331-2294 1848-9710
DOI:	10.15291/geoadria.87