CSCSTI 06.01
BISAC NAT010000
BISAC NAT045050
BISAC NAT025000
BISAC NAT045030
BISAC SCI081000
BISAC SCI092000
BISAC SCI020000
BISAC SCI039000
BISAC SOC053000
BISAC TEC060000
MORPHOMETRIC REGULARITIES OF SUBMARINE SLOPE WITHIN NORTHERN SECTOR OF THE BLACK SEA
Yu. Shuyskiy
Odesskiy nacional'nyy universitet im. I.I.Mechnikova (ONU)
Russian Federation
Abstract:
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.
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.
Keywords:
MORPHOMETRIC REGULARITIES
MORPHOMETRIC REGULARITIES
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