Enhanced rock-slope failure following ice-sheet deglaciation: timing and causes
The temporal pattern of rock-slope failures (RSFs) following Late Pleistocene deglaciation on tectonically stable terrains is controversial: previous studies variously suggest (1) a rapid response due to removal of supporting ice (‘debuttressing’), (2) a progressive decline in RSF frequency, and (3)...
Published in: | Earth Surface Processes and Landforms |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Wiley
2014
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Subjects: | |
Online Access: | http://eprints.gla.ac.uk/129979/ |