Slope instabilities on perennially frozen and glacierised rock walls: multi-scale observations, analyses and modelling

Slope failures from steep bedrock slopes have occurred in mountain areas throughout time. This is a consequence of the topography, geological characteristics, intense freeze-thaw activity and oversteepened slopes from glacier erosion. However, during the past decades, an increased number of periglac...

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Bibliographic Details
Main Author: Fischer, L
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 2009
Subjects:
Online Access:https://www.zora.uzh.ch/id/eprint/31038/
https://www.zora.uzh.ch/id/eprint/31038/1/Fischer_Slope_Instabilities_2009.pdf
https://doi.org/10.5167/uzh-31038