Features of geomorphology and evolution of the North-Eastern shelf of the Black Sea
Abstract
A geomorphological scheme of the shelf of the North-East Black Sea has been compiled, showing submarine terraces, «marginal bar» or system of bars and the shelf's edge. Analysis of the present-day abrasion processes allows concluding that the terraces are regularly formed at depths less than 20 meters and more than 60 to 70 meters. A simple mathematical model of shelf evolution is introduced.
About the Authors
N. V. Esin
Южное отделение Института океанологии им. П. П. Ширшова АН СССР
Russian Federation
Russian Federation
Yu. D. Evsyukov
Южное отделение Института океанологии им. П. П. Ширшова АН СССР
Russian Federation
Russian Federation
M. T. Savin
Южное отделение Института океанологии им. П. П. Ширшова АН СССР
Russian Federation
Russian Federation
V. A. Dmitriev
Южное отделение Института океанологии им. П. П. Ширшова АН СССР
Russian Federation
Russian Federation
Review
For citations:
Esin N.V., Evsyukov Yu.D., Savin M.T., Dmitriev V.A. Features of geomorphology and evolution of the North-Eastern shelf of the Black Sea. Geomorfologiya. 1980;(3):71-76. (In Russ.)
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