Abstract
One of the possible methods for assessing modern geodynamic processes in the development of the earth's surface relief is described. It is based on the analysis of the exogenously active layer. Within its limits, the relief-forming process is studied as a result of the interaction of endogenous and exogenous forces, which occurs under the influence of neotectonic movements. As a result of modeling within the research object, the correspondence of the latest movements and formations was established not only of the Carboniferous-Permian coal-bearing basin, confirmed by gravimetric data, but also of the Permian-Triassic volcano-plutonic province.
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