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...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Mackay, J. Ross
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1981
Subjects:
Ice
Online Access:http://dx.doi.org/10.1139/e81-154
http://www.nrcresearchpress.com/doi/pdf/10.1139/e81-154