Геоморфологический эффект и гидравлика позднеплейстоценовых йокульлаупов ледниково-подпрудных озер Алтая
Аннотация
Catastrophic floods released from enormous Pleistocene glacial lakes transformed essentially the former topography and created an assemblage of erosional and depositional landforms, a kind of alpine scablands, not unlike to the Channeled Scabland of North America. At their peak discharge, the glacial foods due to outbursts of the Chuya-Kurai system of the ice-dammed lakes were about 1 to 18 mln. cub. m per second. Those were the greatest fresh water flows known on the Earth.
Рецензия
Для цитирования:
Рудой А.Н. Геоморфологический эффект и гидравлика позднеплейстоценовых йокульлаупов ледниково-подпрудных озер Алтая. Геоморфология и палеогеография. 1995;(4):61-76.
For citation:
Rudoi A.N. Geomorphic effect and hydraulics of the Late Pleistocene jokulhlaups of ice-dammed lakes in the Altai. Geomorfologiya i Paleogeografiya. 1995;(4):61-76.
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