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oa The importance of an integrated approach in solving scientific and practical issues of geology, geomorphology, paleogeography of the Left Bank of the Middle Dnieper
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, Geoinformatics, May 2021, Volume 2021, p.1 - 6
Abstract
Development of relief and paleogeography of the territory of the hydrographic basin of the Left Bank of the Middle Dnieper in the middle and late Pleistocene in the publications of researchers are most often associated with direct and side effects of the Dnieper glaciation. This applies, in particular, to the problem of restructuring the quaternary hydrographic network of the territory. The glacier squeezed out compensatory shafts, created dams and before him there were glacial pools. These were changed the course of erosion-accumulation processes in the riverbeds, valleys, and the entire basin. This inevitably caused the restructuring of the hydrographic network: intra-valley, intra-system and intersystem structures of the hydrographic system. Glacioisostasis also plays an important role. Specific examples of restructuring is interception collision, upper and lateral collisions. Hydrographic basin of the Left Bank of the Middle Dnieper is located on the Dnieper-Donetsk depression (DDD), which according to a set of geological, geophysical, paleogeographic, paleogeomorphological data is an active geodynamic structure. Studies of various issues of Quaternary geology, geomorphology and paleogeography of the Left Bank of the Middle Dnieper should be conducted on a comprehensive basis, which is created geology, geophysics, paleogeomorphology. It is necessary to take into account and link the results obtained for this area, as well as the results of research in other regions.