Active layer slope movement in a continuous permafrost environment, Garry Island, Northwest Territories, Canada
Field investigations have been carried out at Garry Island, N.W.T. for the 1964–1980 period in order to study downslope active layer movement at sites with two-sided (downward and upward) freezing and active ice-wedge growth. Movements have been determined with reference to semi-flexible plastic tub...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1981
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Online Access: | http://dx.doi.org/10.1139/e81-154 http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-154 |