Geoadria, Vol. 10 No. 2, 2005.
Izvorni znanstveni članak
https://doi.org/10.15291/geoadria.55
Geomorphologic features of the Krka valley and its river basin, with respect to the section from Knin to Bilušić Buk
Dražen Perica
Danijel Orešić
Srećko Trajbar
Sažetak
The Krka River and its tributaries make the system of composite valleys in the karst. The composite valley system is the result of lithologic and tectonic relations. The Krka valley is of polygenetic origin. In the canyon sections there are many characteristic slope relief details. On steeper slopes crumbling and collapsing is significant. The debris of surrounding rocks is found in alluvial deposits at the valley widening. In recent times, the regeneration of vegetation is noticeable, which contributes to decreasing intensity of relief shaping by exogenic processes.
Ključne riječi
Krka River; geomorphologic features; slope processes; anthropogenic and zoogenic influences
Hrčak ID:
9660
URI
Datum izdavanja:
1.12.2005.
Posjeta: 7.552 *