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Black executive dating

Because of the extreme stratification, it is classified as a salt wedge estuary.The Black Sea only experiences water transfer with the Mediterranean Sea, so all inflow and outflow occurs in the Bosphorus and Dardanelles.The geological origins of the basin can be traced back to two distinct relict back-arc basins which were initiated by the splitting of an Albian volcanic arc and the subduction of both the Paleo- and Neo-Tethys Oceans, but the timings of these events remain controversial.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.It is through the most active of these connective routes, the Turkish Straits, that the Black Sea joins the world ocean.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.

The principal Greek name "Póntos Áxeinos" itself is generally accepted to be a rendering of Iranian *axšaina- (“dark colored”), cf.Inflow from the Mediterranean has a higher salinity and density than the outflow, creating the classical estuarine circulation.This means that inflow of dense water from the Mediterranean occurs at the bottom of the basin while outflow of fresher Black Sea surface-water into the Marmara Sea occurs near the surface.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.The Black Sea drains into the Mediterranean Sea, via the Aegean Sea and various straits, and is navigable to the Atlantic Ocean.

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