Basal hydrofractures near sticky patches
Basal crevasses are macroscopic structural discontinuities at the base of ice sheets and glaciers that arise by fracture. Motivated by observations and by the mechanics of elastic fracture, we hypothesise that spatial variations in basal stress (in the presence of basal water pressure) can promote a...
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| Hauptverfasser: | , , , , |
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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Cambridge University Press
2023-06-01
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| Schriftenreihe: | Journal of Glaciology |
| Schlagworte: | |
| Online-Zugang: | https://www.cambridge.org/core/product/identifier/S0022143022000752/type/journal_article |
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