On the exogenous origin of some intermountain basins of the Upper Kolyma Upland
Abstract
Certain relief types similar in morphological features to tectonic intermountain depressions are likely to result from filling Neogene river valleys with glacial deposits. This process was favoured by lower rates of tectonic movements and also by progressive changes in Pleistocene paleoclimates.
Review
For citations:
Bespaly V.G., Rudnev A.V. On the exogenous origin of some intermountain basins of the Upper Kolyma Upland. Geomorfologiya. 1988;(3):83-88.
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