Pregled bibliografske jedinice broj: 458910
The influence of nivation and cryofraction on periglacial relief formation on Velebit Mt. (Croatia)
The influence of nivation and cryofraction on periglacial relief formation on Velebit Mt. (Croatia) // Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society, 63 (2010), 3; 271-282 (međunarodna recenzija, članak, znanstveni)
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Naslov
The influence of nivation and cryofraction on periglacial relief formation on Velebit Mt. (Croatia)
Autori
Perica, Dražen ; Lončar, Nina ; Lozić, Sanja
Izvornik
Geologia Croatica : journal of the Croatian Geological Survey and the Croatian Geological Society (1330-030X) 63
(2010), 3;
271-282
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
nivation ; cryofraction ; periglacial relief ; Velebit Mt. ; Croatia
Sažetak
The studied peak areas of the Velebit Mt. display a interesting periglacial geomorphology. The appearance of forms is the result of the interdependent geological, geomorphologic, climatic, vegetational and pedological characteristics of the area. The structural and litological properties of the rock complex, and the inclination of the slope, play a significant role in periglacial relief modelling. Climatic elements are also important, as they influence the intensity and duration of the processes. Low temperatures and relatively high amount of precipitation during the last ice age (Würm III) served to intensive activity of periglacial processes and relief modelling of the entire Velebit Mt. area. Nivation and cryofraction are the most expressive of all periglacial processes which are represented by snow avalanches, snow accumulations, stone streams etc. Air temperatures and soil temperatures (at 30, 60, 90 cm) are mesaured, presented and reviewd together other atributes and slope inclination of the area. The interactions between ground temperature, snow cower and wind patterns play important role to frost actions. In addition to inclination, the penetration of warm winds (jugo) and warming of snow on the NE slopes are also important factors in destabilizing the snow cover and triggering avalanches. GIS analysis of slope of the area in question was applied during quantitative geomorphologic analysis. Snow avalanches are the most intensive on the slopes with declinations from 35° up to 50°, especially on the parts without vegetation cover.
Izvorni jezik
Engleski
Znanstvena područja
Geografija
POVEZANOST RADA
Projekti:
MZOS-119-0000000-1299 - Geomorfološko kartiranje Republike Hrvatske (Buzjak, Nenad, MZOS ) ( CroRIS)
MZOS-269-2693084-3083 - Hrvatski priobalni krški prostor - geomorfološke i ekološke značajke (Perica, Dražen, MZOS ) ( CroRIS)
Ustanove:
Sveučilište u Zadru
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus
Uključenost u ostale bibliografske baze podataka::
- Geobase
- GeoRef