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. OstaninRussian Federation
R. R. Atlasov
Russian Federation
V. A. Bukreev
Russian Federation
N. B. Levina
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.)