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Subinertial motions over the Northeastern shelf of the Black Sea

โœ Scribed by G. G. Matishov, Yu. I. Inzhebeikin


Book ID
120813103
Publisher
SP MAIK Nauka/Interperiodica
Year
2012
Tongue
English
Weight
237 KB
Volume
446
Category
Article
ISSN
1028-334X

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During latest Quaternary glaciation, the Black Sea became a giant freshwater lake. The surface of this lake drew down to levels more than 100 m below its outlet. When the Mediterranean rose to the Bosporus sill at 7,150 yr BP', saltwater poured through this spillway to refill the lake and submerge,