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Геоморфология и палеогеография

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Геоморфология Шахунских Увалов

Аннотация

A large orographic unit - Shakhunsky Uvaly - is known in NE Gorki region, within the Vetluga drainage basin. By hypsometric position, relief and geology of the unit it can be considered as a series of remnants of planation surface, dominating at present the northern Privolzhskaya upland, earlier it spread further northward. The Vetluga region morphostructure reflects consequent stages of the structural-tectonic evolution. The Shakhunsky Uvaly is formed long before the Dnieper Ice Age. During the whole Cenozoic it controlled the spatial distribution of the morphosculptural elements, including pre-glacial, glacial and post-glacial forms.

Об авторе

Б. И. Фридман
Средневолжская комплексная геологоразведочная экспедиция
Россия


Рецензия

Для цитирования:


Фридман Б.И. Геоморфология Шахунских Увалов. Геоморфология. 1981;(3):85-91.

For citation:


Fridman B.I. Geomorphology of the Shakhunsky Uvals. Geomorfologiya. 1981;(3):85-91.

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ISSN 2949-1789 (Print)
ISSN 2949-1797 (Online)