Geomorphic evidence for present-day snow-avalanche and debris-flow impact in the Icelandic Westfjords

被引:55
作者
Decaulne, Armelle
Saemundsson, Thorsteinn
机构
[1] Nat Res Ctr NW Iceland, IS-550 Saudarkrokur, Iceland
[2] Univ Blaise Pascal, CNRS, UMR 6042, Geolab, F-63057 Clermont Ferrand 1, France
关键词
snow avalanches; debris flows; geomorphic efficiency; fjords; Iceland;
D O I
10.1016/j.geomorph.2005.09.007
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The geomorphic impact of present-day processes on slopes, with emphasis on the impact of snow avalanches and debris flows, is investigated in North-western Iceland. Data are obtained from topographical maps, aerial photographs and field survey, as well as from measurements of talus characteristics and estimates of the volumes of recent deposits. The impact of various kinds of snow avalanches (dry and wet slab avalanches and slush flows) that have occurred recently in the area is shown. The effects of avalanches, including material transport and avalanche boulder tongue development, and the resulting landforms are identified and analysed. The geomorphic significance of debris flows is also examined, their deposits described and erosional and depositional landforms (channels, levees and lobes) measured. The geomorphological impact in the Icelandic Westfords area is discussed in relation to research in other environments. Observations indicate that snow avalanches are locally significant but their impact on talus slopes and talus cones where there are also debris-flow deposits is moderate. In contrary debris-flow deposits are a strong geomorphic agent on slopes. (c) 2006 Elsevier B.V. All rights reserved.
引用
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页码:80 / 93
页数:14
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