This paper interprets glacial and periglacial processes within the Mackenzie River valley on the basis of the delineation of transverse valley-profiles. The Mackenzie River courses from Great Slave Lake in the southwest to the Mackenzie Delta on the Arctic coast in the northwest of the Northwest Territories.
Discussion Paper no. 19.
Copyright is held by the author(s) and the Dept. of Geography, Simon Fraser University.
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