CSCSTI
06.01
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BISAC
NAT010000
NAT045050
NAT025000
NAT045030
SCI081000
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SCI039000
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TEC060000
MORPHOMETRIC REGULARITIES OF SUBMARINE SLOPE WITHIN NORTHERN SECTOR OF THE BLACK SEA
Authors:
1.
Odesskiy nacional'nyy universitet im. I.I.Mechnikova (ONU)
Russian Federation
Russian Federation
Type:
Conference article
Pages:
from 372
to 376
Published:
24.11.2012
Subject area:
CSCSTI 06.01
BISAC NAT010000 Ecology
BISAC NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAC NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAC NAT045030 Ecosystems & Habitats / Polar Regions
BISAC SCI081000 Earth Sciences / Hydrology
BISAC SCI092000 Global Warming & Climate Change
BISAC SCI020000 Life Sciences / Ecology
BISAC SCI039000 Life Sciences / Marine Biology
BISAC SOC053000 Regional Studies
BISAC TEC060000 Marine & Naval
BISAC NAT010000 Ecology
BISAC NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAC NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAC NAT045030 Ecosystems & Habitats / Polar Regions
BISAC SCI081000 Earth Sciences / Hydrology
BISAC SCI092000 Global Warming & Climate Change
BISAC SCI020000 Life Sciences / Ecology
BISAC SCI039000 Life Sciences / Marine Biology
BISAC SOC053000 Regional Studies
BISAC TEC060000 Marine & Naval
Language:
Russian, English
Keywords:
MORPHOMETRIC REGULARITIES
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
1. net spiska literatury
