Glaciolacustrine terrace in the Izborsko-Malskaya valley: structure, age and mechanism of formation
https://doi.org/10.31857/S0435428122010084
Abstract
Using the Izborsko-Malskaya valley (Pskov region) as an example was considered the issues of the origin of glaciolacustrine terraces in overdeepened valleys widespread in the Late Valdai (Ostashkov, Weichselian) glaciations areas. Fragments of the one-levelled terrace in the northern part of the Izborsko-Malskaya valley, composed of fine-laminated sands, are adjacent to the lower parts of the valley slopes. This terrace could be determined as alluvial or kame terrace. Detail field and lab investigations allowed us to establish the formation of fine-laminated sands. They accumulated in the proglacial lake during the Izborsko-Malskayay valley’s deglaciation. Then the sandy thickness was divided by the water flow. The formation of the erosional incision should not be associated with the modern r. Obdekh. It tooks a more significant water flow then in the modern river. Perhaps the dissection of the primary glaciolacustrine surface and the initiation of an erosion cut in the bottom of the valley occurred during the proglacial lake discharge ~ 13.3 ka. The ice-dammed drainage happened rather quickly. That is why there is no variability in the composition and facies in the upper part of the glaciolacustrine deposits. Furthermore, the additional terraces are absent in the erosion incision. Thus, the surfaces of terrace fragments have an accumulative glaciolacustrine origin and their scarps - erosional genesis. The new data on the mechanism formation of terraces in the northwest of the East European Plain differ from current concepts. Along with the previously described mechanisms of glaciolacustrine terraces formation (abrasion activity of former proglacial lakes, gradual cutting of rivers, or the formation of slopes of glacial contact in kame terraces), one should bear in mind the possibility of cutting powerful water flows during catastrophic discharges of proglacial lakes. The investigation results indicate the necessity for detailed studies in valleys on the northwest of the East European Plain.
Keywords
About the Authors
N. V. KarpukhinaRussian Federation
Moscow
A. N. Makkaveyev
Russian Federation
Moscow
A. L. Zakharov
Russian Federation
Moscow
E. A. Konstantinov
Russian Federation
Moscow
R. N. Kurbanov
Russian Federation
Faculty of Geography, Lomonosov Moscow State University
Moscow
S. S. Bricheva
Russian Federation
Faculty of Geography, Lomonosov Moscow State University
Moscow
N. V. Sychev
Russian Federation
Moscow
D. V. Baranov
Russian Federation
Moscow
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Review
For citations:
Karpukhina N.V., Makkaveyev A.N., Zakharov A.L., Konstantinov E.A., Kurbanov R.N., Bricheva S.S., Sychev N.V., Baranov D.V. Glaciolacustrine terrace in the Izborsko-Malskaya valley: structure, age and mechanism of formation. Geomorfologiya. 2022;53(1):65-80. (In Russ.) https://doi.org/10.31857/S0435428122010084