geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2227Research ArticleНаучные сообщенияShort communicationsНекоторые черты геоморфологии и эволюции шельфа северо-восточной части Черного моряFeatures of geomorphology and evolution of the North-Eastern shelf of the Black SeaЕсинН. В.EsinN. V.ЕвсюковЮ. Д.EvsyukovYu. D.СавинМ. Т.SavinM. T.ДмитриевВ. А.DmitrievV. A.Южное отделение Института океанологии им. П. П. Ширшова АН СССРРоссия19800709202203Геоморфология7176Copyright © Есин Н.В., Евсюков Ю.Д., Савин М.Т., Дмитриев В.А., 20222022Есин Н.В., Евсюков Ю.Д., Савин М.Т., Дмитриев В.А.Esin N.V., Evsyukov Y.D., Savin M.T., Dmitriev V.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2227

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.

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.

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The authors declare that there are no conflicts of interest present.