Molards as an indicator of permafrost degradation and landslide processes
Molards have been defined in the past as conical mounds of debris that can form part of a landslide’s deposits. We present the first conclusive evidence that molards in permafrost terrains are cones of loose debris that result from thawing of frozen blocks of ice-rich sediments mobilised by a landsl...
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| Main Authors: | , , , , , , , , |
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| Format: | Default Article |
| Published: |
2019
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| Subjects: | |
| Online Access: | https://hdl.handle.net/2134/37446 |
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