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Geomorfologiya i Paleogeografiya

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Marginal features and boundery of the Valdai ice sheet at the Vaga drainage basin

Abstract

Marginal features and boundaries of maximum and Vepsovo stages of the Valdai glaciation are described within the Vaga drainage basin, the forms being identified by aiephotographs interpretation and special field studies. Both petrography of gravels and boulders in the Valdai and Moscow tills and mineralogy of the tills corroborate the position of the Valdai ice sheet boundary established by geomorphic data.

About the Authors

V. E. Ostanin
Всесоюзное научно-производственное объединение «Аэрогеология»
Russian Federation


R. R. Atlasov
Всесоюзное научно-производственное объединение «Аэрогеология»
Russian Federation


V. A. Bukreev
Всесоюзное научно-производственное объединение «Аэрогеология»
Russian Federation


N. B. Levina
Всесоюзное научно-производственное объединение «Аэрогеология»
Russian Federation


Review

For citations:


Ostanin V.E., Atlasov R.R., Bukreev V.A., Levina N.B. Marginal features and boundery of the Valdai ice sheet at the Vaga drainage basin. Geomorfologiya. 1979;(1):72-76. (In Russ.)

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