Water Expulsion and Pingo Formation in a Region Affected by Subsidence
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Abstract Geophysical evidence indicates that the delta area of the Mackenzie River, Northwest Territories, is affected by tectonic subsidence. Pingos are of sparse occurrence in the Arctic as a whole but they occur in hundreds in the Mackenzie River delta. In a region of subsidence, as recent sediments pass through the base of permafrost, compaction becomes possible. The resulting water expulsion produces an artesian head responsible for building pingos.
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2014 ◽
Vol 458
(1)
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pp. 1047-1051
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2007 ◽
Vol 34
(23)
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pp. n/a-n/a
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1986 ◽
Vol 22
(3)
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pp. 440-442
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