Abstract and keywords
Abstract (English):
In northern part of the Black Sea Submarine Slope are anthropogenous age, that formed in different paleogeographical, geological, hydrogenous, lithodynamical, climatic and other conditions. As a result, different forms, declivities and deeps of the slope profiles made up along various sites of the Black Sea coastal zone. Wide spectra of profile forms were detected: straight, curved complex, sinuous, salient, concave, convexo-concave. A underwater slope gradients are different, from 0,5 to 0,002 in depend of different conditions and geological history. The submarine slope researches were executed from Danube delta on the West to Khersoness Cape on the East on 192 sites, approximately 300 crossing profiles were measured up to 8–13 m depth in the coastal zone.


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