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...

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Bibliographic Details
Published in:Collection EDYTEM. Cahiers de géographie
Main Authors: Ravanel, Ludovic, Malet, Emmanuel, Duvillard, Pierre-Alain, Magnin, Florence, Deline, Philip, Guillet, Grégoire, Troilo, Fabrizio, Pogliotti, Paolo, Morra di Cella, Umberto, Beutel, Jan, Gruber, Stephan
Format: Article in Journal/Newspaper
Language:French
Published: Le Bourget-du-Lac : Laboratoire EDYTEM 2017
Subjects:
geo
Ice
Online Access:https://doi.org/10.3406/edyte.2017.1360
https://www.persee.fr/doc/edyte_1762-4304_2017_num_19_1_1360