Instrumentation thermique et cinématique des parois à permafrost du massif du Mont Blanc
Unlike the superficial deposits in which the presence of permafrost is indicated by geomorphological evidences, its occurrence in the rock walls can only be suggested by the existence of perennial ice sheets or hanging glaciers. Everywhere else, only indirect (geophysics) or direct temperature measu...
Published in: | Collection EDYTEM. Cahiers de géographie |
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Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | French |
Published: |
Le Bourget-du-Lac : Laboratoire EDYTEM
2017
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Subjects: | |
Online Access: | https://doi.org/10.3406/edyte.2017.1360 https://www.persee.fr/doc/edyte_1762-4304_2017_num_19_1_1360 |