Komagorova M.A.

THE STATE OF THE ART AND NEW DATA ON THE RELIEF AND QUATERNARY GEOLOGICAL STRUCTURE OF THE VALDAI UPLAND WESTERN PERIPHERY 

Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9.

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doi: 10.24412/2687-1092-2022-9-333-338

A.E. Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia 

 

     

Abstract. The history of geological study and mapping of the Toropetsky district of the Tver region is briefly described. It is shown that at the moment there is not a single published geological map larger than the scale of 1:1000000 for the studied area. The results of the study of the relief bearing traces of geological events during the degradation of the last Valdai glaciation are presented.

Keywords: marginal moraines, Valdai upland, northwest of Tver region, degradation of the Valdai glaciation, glaciofluvial sediments


 

REFERENCES:

Butakov P.M., Savanin V.V., Kamyarya V.V., Menshikova O.V. etc. State geological map of the Russian Federation. Scale 1: 200,000. Second edition. Ilmenskaya series. Sheet O-36-XXVI (Kholmskaya Square). Explanatory letter. St. Petersburg: Cartographic factory VSEGEI, 2017, 185 p. (In Russ.)

Verbitsky V.R., Verbitsky I.V., Vasilyeva O.V., Savanin V.V. and others. State Geological Map of the Russian Federation: scale 1:1,000,000 (third generation). Series Central European. Explanatory letter. Sheet O-35: Pskov, (N-35), O-36: St. Petersburg. St. Petersburg, VSEGEI, 2012. 508 p. (In Russ.)

Dorofeev A.A., Khokhlova E.R. Landscapes of the Tver region: monograph. Tver: Tver. state un-t, 2016. p. 73. (In Russ.)

Geology of the USSR. M., 1971. T. 1: Leningrad, Pskov and Novgorod regions. Geological description; Plains of the European part of the USSR. M., 1974 (In Russ.)

 

Cite this article:

Komagorova M.A. 2022. The state of the art and new data on the relief and quaternary geological structure of the Valdai High western periphery // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 333-338. doi: 10.24412/2687-1092-2022-9-333-338

 

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