Abstract
The analysis and comparison of the morphology of stone fields by Syvulyanskyi and Dovbushanskyi ridges of Skybovi Gorgany have been made. Morphometric characteristics, mechanism of formation, age and current state have been considered according to their relative distribution on the slopes. Conclusions, based on the paleogeographic conditions of their formation have been made. Key words: stone fields, slope, roundness, Gorgany, orientation of fragments.
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