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Rock stream deserption


, : Rock stream deserption. International Conference on Permafrost, Proceedings 4(Pages 1078-1082

The authors have investigated rock streams by analyzing the frozen materials of which they are composed. On the basis of abundant data it was shown that rock streams are not chaotic accumulations of coarse material as was earlier considered but orderly geodynamic systems evolving according to certain rules. Three hypsometric belts have been distinguished, merging oneinto the next in orderly fashion. Each of these belts consists of a strictly defined combination of facies and subfacies differing both in structure and in the range of factors affecting its movement. The range of sediments occurring in a rock stream depends on its genesis, stage of development, and geological and geomorphological peculiarities.--Modified journal abstract.

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