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ПРОИСХОЖДЕНИЕ “ВРЕЗАННЫХˮ ИЛИ СЛЕПЫХ ДЕЛЬТ НА ВОЛГО-УРАЛЬСКОМ МЕЖДУРЕЧЬЕ В СВЕТЕ НОВЫХ ПРЕДСТАВЛЕНИЙ ОБ ИСТОРИИ КОЛЕБАНИЙ УРОВНЯ КАСПИЯ

Published in Geomorphology RAS • Jan 1, 2020
NobleIDNI1P35W23R45S22
Authors:
Е.Н. Бадюкова

Abstract

The relief of the Volga-Ural interfluve is considered, where the rivers in the mouths form “embedded” or blind deltas. These deltas terminate close to the Volga-Ural Sands. During spring snowmelt floods, large lakes appear at the mouths of rivers. Therefore, it is difficult to agree with the opinion...

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