Geology, glacier retreat and permafrost degradation as controlling factors of slope instabilities in a high-mountain rock wall: the Monte Rosa east face

The Monte Rosa east face, Italian Alps, is one of the highest flanks in the Alps (2200–4500 m a.s.l.). Steep hanging glaciers and permafrost cover large parts of the wall. Since the end of the Little Ice Age (about 1850), the hanging glaciers and firn fields have retreated continuously. Du...

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Bibliographic Details
Main Authors: L. Fischer, A. Kääb, C. Huggel, J. Noetzli
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/6/761/2006/nhess-6-761-2006.pdf