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...
| Published in: | Geosciences |
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| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2021-10-01
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| Subjects: | |
| Online Access: | https://www.mdpi.com/2076-3263/11/10/417 |