The mapping approach based on revealed property of the geodynamical memory of actual soil cover (Holocene) is realized. Structure and facies of the soil cover are considered as a new information donor about the relief dynamics. The raw of tectogenic evolution of the soil-forming processes and the soil types in the range from subsidences to stable regime and elevations with different intensity is determined. For the Western Volyno-Podillya and Pre-Carpathian foredeep the calibration raw “soil type – total amplitude of vertical movements” is justified. On it’s basis first the Map of vertical Holocene movements in scale 1:500000 with entire covering of the terrain is composed and interpreted. The differentiatial movements’ regimes of the map are compared with the data about the region’s morphostructures obtained by geology-geomorphological methods.
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