Crevasse-induced Rayleigh-wave azimuthal anisotropy on Glacier de la Plaine Morte, Switzerland

Crevasses and englacial fracture networks route meltwater from a glacier's surface to the subglacial drainage system and thus influence glacial hydraulics. However, rapid fracture growth may also lead to sudden and potentially hazardous structural failure of unstable glaciers and ice dams, rift...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Lindner, F., Laske, G., Walter, F., Doran, A.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003669