Calculating the cohesion and internal friction angle of volcanic rocks and rock masses
Rock failure criteria are key input parameters for models designed to better understand the stability of volcanic rock masses. Cohesion and friction angle are the two defining material variables for the Mohr-Coulomb failure criterion. Although these can be determined from laboratory deformation expe...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Volcanica
2021-11-01
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| Series: | Volcanica |
| Subjects: | |
| Online Access: | https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/134 |