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The morphostructure of an crest part of the Voronezh anteclise is closely related to the neotectonics of the territory. A feature of the newest structure, in contrast to the Paleozoic, Mesozoic and Paleogene structures, is predominantly the submeridional orientation of the interchanging raised and downdip blocks. The following regularities of the degree of the reflection of the deep inhomogeneities in neotectonic and geomorphological characteristics have been revealed. The zones of the reduceddoi:10.32454/0016-7762-2017-5-13-19 fatcat:7bv2kbawxzf5jgybeb4sseze4q