Rock Glacier Dynamics by a Thermo-Elastic-Viscoplastic Constitutive Relationship

As a result of mountain permafrost creep, rock glaciers are common features in high-altitude periglacial areas. From a practical point of view, beyond their localization and inventorying, both the monitoring and prediction of their evolution due to climate changes are crucial. One of the effects of...

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Bibliographic Details
Main Authors: Stefano Alberti, Luca Flessati
Format: Article
Language:English
Published: MDPI AG 2021-10-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/10/417