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. During recen...

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Bibliographic Details
Published in:Natural Hazards and Earth System Sciences
Main Authors: Fischer, L., Kääb, A., Huggel, C., Noetzli, J.
Format: Text
Language:English
Published: 2018
Subjects:
Ice
Online Access:https://doi.org/10.5194/nhess-6-761-2006
https://nhess.copernicus.org/articles/6/761/2006/