Fluvioglacial deposits in large lakes and inland seas of the eastern periphery of the Baltic Shield: formation peculiarities, lithological features and place in the palaeogeography of the Late Pleistocene-Holocene in the Northwest European part of Russia
DOI:
https://doi.org/10.31951/2658-3518-2024-A-4-630Keywords:
Ladoga and Onega Lakes, White and Baltic Seas, ice sheet degradation, limno-glacial sediments, glacial-marine sediments, seismoacoustic profilingAbstract
In the report, on the basis of studies of the Quaternary cover of the Ladoga and Onega lakes and the White Sea carried out in the last decade, the question of the peculiarities of the formation of the first glacial lakes on the eastern periphery of the Baltic crystalline shield, the time of their deposition, and the peculiarities of sedimentogenesis is discussed. It is concluded that sediments of a specific type of sedimentation, which are formed everywhere in inland basins (seas and lakes) can be identified as a glacial-water formation specific to the glacial regions of the Earth.
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This work is distributed under the Creative Commons Attribution-NonCommercial 4.0 International License.