Linear-Patterned Slopes in the Discontinuous Permafrost Zone of the Central Mackenzie River Valley
In the Mackenzie River Valley between Norman Wells and Fort Simpson a study of the character, distribution and orientation of gently-inclined, linear-patterned slopes revealed that most northeast-facing, lichen-covered slopes have permafrost within about 10-25 inches of the surface, and display evid...
Published in: | ARCTIC |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The Arctic Institute of North America
1974
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Subjects: | |
Online Access: | https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65935 |