Abstract

The article analyzes the most expressive indicative features of exogenous geomorphologic processes in assessing their role in the transformation of soil cover. Each of the above-mentioned geomorphologic processes is capable of creating in the process of its activity a material mass that can subsequently become a parent species of a certain variety of soil, and the direction and intensity of processes are the basis for assessing the rates of mechanical degradation of soils. It has been established that the spectrum of modern exogenous processes is significant and multifactorial in terms of its manifestation and development, which leads to the need for their recognition and evaluation in the formation, use and transformation of soil cover. Characterized how the massive masses formed by certain geomorphologic processes in the investigated area, in one way or another, influence the formation of varieties of soil differentiation of the region. An attempt has been made to establish the existing, expected and assume the probable impact of a certain geomorphologic process on soil characteristics, which indicates the prospect of ecological and geomorphologic evaluation of the formation, distribution, operation and transformation of the soil cover of the Northern Black Sea coast. This attempt to explain the correlation of the dynamics of forms of relief and the state of soil cover follows from the new methodical approach of taking into account when assessing the correlation of the main properties of the terrain topography. It has been established that modern exogenous geomorphologic processes, due to their activities of denudation, transit and accumulative nature, carry out the constant production of material masses, are an important factor in the formation of soils, taking them into account gives a much more detailed picture of the distribution of differences in the soil cover of the Northern Black Sea region. In the studied territory, the spectrum of modern exogenous processes is significant (deluvial, gravitational complex, linear erosion, fluvial accumulation, karst, subsidence and gleying, suffusion, abrasion, estuary accumulation and multifactorial in manifestation and development, which leads to the need for their recognition and evaluation in the formation, use and transformation of the soil cover. There are morphological, genetic, age and dynamic signs that the material masses that are formed by certain geomorphological processes in the studied area, one way or another, influence the formation of varieties of soil differences in the region. Key words: modern exogenous geomorphologic processes, soil cover; indicative signs; the Northern Black Sea region; correlation of the dynamics of landforms and the state of the soil cover.

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