Water flow timing, quantity, and sources in a fractured high mountain permafrost rock wall
<p>Water flow in high mountain rock walls is crucial for landscape evolution and slope stability. However, the timing, quantity, and sources of this flow remain poorly understood. In the Mont Blanc massif, tunnels at the Aiguille du Midi peak (3842 m) provide direct access to steep permafrost-affect...
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| Autors principals: | , , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Copernicus Publications
2026-03-01
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| Col·lecció: | Hydrology and Earth System Sciences |
| Accés en línia: | https://hess.copernicus.org/articles/30/1735/2026/hess-30-1735-2026.pdf |
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