I. 3. PEDOGENIC STUDIES ON SOILS CONTAINING PERMAFROST IN THE MACKENZIE RIVER BASIN
In this paper, the Mackenzie River 'bas in i s defined a s the portion that l i e s north of the approximate southern l imit of discon-tinuous permafros t, e a s t of the main mass 'o f the Cordillera, and west of a line joining F o r t Smith, Yellowknife, F o r t Frankl in a t the wes ter...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.971 http://pubs.aina.ucalgary.ca/cpc/cpc1-37.pdf |