Abstract
We obtained new data about the high degree of relationship between the relief and the nature of the latest movements within the depressions of the Ladoga and Onega lakes as a result of geomorphological studies. Computer geodynamic modeling showed that this relationship is explainable by the development of the supposed active faults identified by us on a detailed scale in an environment of northeastern extension, the axis of which is oriented across the strike of the considered lake basins.
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