Russian Federation
NAT010000
NAT045050
NAT025000
NAT045030
SCI081000
SCI092000
SCI020000
SCI039000
SOC053000
TEC060000
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.
MORPHOMETRIC REGULARITIES
1. net spiska literatury