About the possible existence of the Selizharovo proglacial lake
Authors
-
Baranov D.V.
1
- Panin A.V. 1
- Karpukhina N.V. 1 1 Institute of geography RAS, Moscow, Russia
DOI:
https://doi.org/10.31951/2658-3518-2024-A-4-234Keywords:
Volga River, incision valley, Proglacial Lake, Late Valdai glaciationAbstract
The formation of the incision valley near Selizharovo is associated with the existence of a proglacial lake in the Late Valdai. Geological and hypsometric data indicate its possible level is not lower than 205 m and not higher than 210 m asl. However, at this level of the lake, a incision would not be possible, since the edges of the valley are located at an altitude of 215 – 220 m asl. We assume that the depression at Selizharovo already existed by the beginning of the Late Valdai, and then it deepened and was renewed.
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This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
This work is distributed under the Creative Commons Attribution-NonCommercial 4.0 International License.
