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Two hypothetical flood scenarios have been proposed for the Black Sea, describing events that may have profoundly affected prehistoric settlement in Eastern Europe and adjacent parts of Asia. Th e first, a Late Pleistocene ‘Great Flood’ (Chepalyga 2003, 2007), suggests that the brackish Neoeuxinian Lake in the Black Sea basin was rapidly inundated by Caspian Sea overflow via the Manych Spillway shortly after the Late Glacial Maximum (LGM), c. 17–14 ka BP. Th e second, an Early Holocene
- Author
- Jackson LaRose
- Language
- EN