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Rock Glacier Dynamics by a Thermo-Elastic-Viscoplastic Constitutive Relationship
2021
Geosciences
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 climate change is the thickening of the basal shear zone (the portion of the rock glacier where most deformations are localized), eventually leading to the development of unexpected and unprecedented
doi:10.3390/geosciences11100417
fatcat:it2uhjvksjdndltda4t52ekdn4