The Levantine Sea, is the easternmost part of the Mediterranean Sea
The Levantine Sea is bordered by Turkey
in the north and north-east corner
and the Gaza Strip
in the east, Egypt
in the south, and the Aegean Sea
in the northwest. Where it is used as a term its western border is amorphous hence Mediterranean is more commonly used. The open western border to the next part of the Mediterranean (the Libyan Sea
) is defined as a line from headland Ras al-Helal
, south of the western half of Crete
The largest island in its subset of water is Cyprus
. The greatest depth of is found in the Pliny Trench, about south of Crete. The Levantine Sea covers .
The northern part of the Levantine Sea between Cyprus and Turkey can be further specified as the Cilician Sea
, a term more arcane. Also in the north are two large bays, the Gulf of İskenderun
(to the northeast) and the Gulf of Antalya
(to the northwest).
The Leviathan gas field
is quite central in the south-eastern corner, the Levantine Basin.
To the west of the Levantine Deep Marine Basin is the Nile Delta
Basin, followed by the Herodotus Basin
, large and up to deep, which – at a possible age of 340 million years – is believed to be the oldest known ocean crust worldwide.Ben-Gurion University of the Negev: Three Hundred Million Years Under the Sea
The Suez Canal was completed in 1869, linking the Levantine Sea to the Red Sea – and mainly for large vessels. The Red Sea sits a little higher than the Eastern Mediterranean, so the canal is an intermittent tidal strait discharging water into the Mediterranean. The Bitter Lakes – hypersaline natural lakes, interacting with the canal – were a bar to migration of Red Sea species northward for many decades, but as their salinity has virtually equalized with that of the Red Sea, the barrier to migration was removed, and plants and animals from the Red Sea have begun to colonize the eastern Mediterranean. This is the Lessepsian migration, after Ferdinand de Lesseps, the chief engineer of the canal.
Most of the river discharge is from the Nile. Since the Aswan High Dam sits across the river in the 1960s it has facilitated the multiplication of Egyptian agriculture and population. It has reduced, to the sea, the flow of freshwater, mountainous minerals in the silt, and the distance traveled by silt (before this, borne by flood water). This makes the sea slightly saltier and nutrient-poorer than before. This has decimated the morning sardine litorine haul in nets but favoured many Red Sea species.
*Kubin, Elisabeth; Poulain, Pierre-Marie; Mauri, Elena; Menna, Milena; Notarstefano, Giulio. 2019. "Levantine Intermediate and Levantine Deep Water Formation: An Argo Float Study from 2001 to 2017" Water 11, no. 9: 1781. https://doi.org/10.3390/w11091781
*Özsoy, E. and H. Güngör (1993). The Northern Levantine Sea Circulation Based on Combined Analysis of CTD and ADCP Data, In: P. Brasseur (editor), Data Assimilation: Tools for Modelling the Ocean in a Global Change Perspective, NATO ASI Seeries, Springer-Verlag, Berlin.
*Sur, H. İ., Özsoy, E., and Ü. Ünlüata, (1992). Simultaneous Deep and Intermediate Depth Convection in the Northern Levantine Sea, Winter 1992, Ocean.
Study and Analysis of Water Masses Formation in the Levantine Sea
Long Term Ecological Research
Category:Marginal seas of the Mediterranean
Category:Seas of Turkey
Category:Bodies of water of Syria
Category:Bodies of water of Lebanon
Category:Bodies of water of Israel
Category:Bodies of water of Egypt
Category:Bodies of water of Libya
Category:Bodies of water of the State of Palestine
Category:Ecoregions of Cyprus
Category:Ecoregions of Egypt
Category:Ecoregions of Israel
Category:Ecoregions of Lebanon
Category:Ecoregions of Syria
Category:Ecoregions of Turkey
Category:Seas of Africa
Category:Seas of Asia