О некоторых особенности развития речных долин
Аннотация
The fluvial process essence is that it proceeds in reciprocate manner, not in two, but in three dimensions. Alluviation follows erosion and completes every individual stage, while the stages repeat themselves continuously. The valley deepening into solid rocks (when considered in integral form) proceeds, in a way, through the bedload layer.
Рецензия
Для цитирования:
Скоморохов А.И. О некоторых особенности развития речных долин. Геоморфология и палеогеография. 1995;(1):23-29.
For citation:
Skomorokhov A.I. On some special features in the river valleys evolution. Geomorfologiya i Paleogeografiya. 1995;(1):23-29.
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