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Genesis and structure of soil cover on marine abrasion-accumulation terraces in southern Dagestan



Genesis and structure of soil cover on marine abrasion-accumulation terraces in southern Dagestan



Vestnik Moskovskogo Universiteta, Seriya 17, Pochvovedeniye Moscow



The soil cover structure is considered on the basis of vast cartographic material, chemical characteristics of soil toposequences and statistical treatment of the data obtained as related to the lithology, topography, evolution and tectonics of the area. The trends in soil cover evolution on marine terraces are thought to be different within anticlinal and synclinal zones, hydromorphic stage of soil cover development being much more prolonged within synclinal zone. Under the influence of anthropogenic effect the soil cover goes back to the previous stages of evolution.

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