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Mediterranean water flows into the Black Sea as part of a two-way hydrological exchange.
The Black Sea outflow is cooler and less saline, and floats over the warm, more saline Mediterranean inflow – as a result of differences in density caused by differences in salinity – leading to a significant anoxic layer well below the surface waters.
According to the same explanation and reasoning, it is therefore considered to be impossible for the Scythians (who principally roamed in what is present-day Ukraine and Russia) to have given the designation as they lived to the north of the sea, and it would be therefore a southern antipodal body of water for them.
As the name could have only been given by a people that were well aware of both the northern "black/dark" and southern "red" seas, it is therefore considered probable that it was given its name by the Achaemenids (550–330 BC). He also thought that the Black Sea was called "inhospitable" before Greek colonization because it was difficult to navigate, and because its shores were inhabited by savage tribes.(7.3.6) The name was changed to "hospitable" after the Milesians had colonized the southern shoreline, the Pontus, making it part of Greek civilization.
These waters separate Eastern Europe, the Caucasus and Western Asia.
The Black Sea is also connected to the Sea of Azov by the Strait of Kerch. Due to these variations in the water level in the basin, the surrounding shelf and associated aprons have sometimes been land.
Since its initiation, compressional tectonic environments led to subsidence in the basin, interspersed with extensional phases resulting in large-scale volcanism and numerous orogenies, causing the uplift of the Greater Caucasus, Pontides, Southern Crimean Peninsula and Balkanides mountain ranges.
Old Georgian sources of 9th–14th centuries ("The Georgian Chronicles") were using the name "Speris Zğua" (სპერის ზღუა), which means "The Sea of Speri", after the name of Kartvelian tribe Speris or Saspers, now in Turkey.
The southern edge around Turkey and the eastern edge around Georgia, however, are typified by a narrow shelf that rarely exceeds 20 km (12 mi) in width and a steep apron that is typically gradient with numerous submarine canyons and channel extensions.
The Euxine abyssal plain in the centre of the Black Sea reaches a maximum depth of 2,212 metres (7,257.22 feet) just south of Yalta on the Crimean Peninsula.
When this hydrological link is not present, the Black Sea is an endorheic basin, operating independently of the global ocean system, like the Caspian Sea for example.
Currently the Black Sea water level is relatively high, thus water is being exchanged with the Mediterranean.
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