Variations in surface area of six ice aprons in the Mont-Blanc massif since the Little Ice Age

Deglaciation of high mountain rockwalls alters slope stability as rockwalls become more sensitive to modifications in environmental factors (e.g. seasonal temperature variations). In the past decades, increasing efforts focused on studying deglaciated Alpine rockwalls. Yet, currently deglaciating ro...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Grégoire Guillet, Ludovic Ravanel
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2020
Subjects:
Online Access:https://doi.org/10.1017/jog.2020.46
https://doaj.org/article/d9dd23f554834f9abd5e914ae0773faa