An analysis of the stability of thawing slopes, Ellesmere Island, Nunavut, Canada
Active-layer detachment slides are locally common on Fosheim Peninsula, Ellesmere Island, where permafrost is continuous, the active layer is 0.5-0.75 m thick, and summer temperatures are unusually high in comparison with much of the Canadian High Arctic. In this paper we report pore-water pressures...
| Published in: | Canadian Geotechnical Journal |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Canadian Science Publishing
2000
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1139/t99-118 http://www.nrcresearchpress.com/doi/pdf/10.1139/t99-118 |