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Gulf of Suez

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Gulf of Suez
NameGulf of Suez
CaptionMap showing the Gulf of Suez.
LocationRed Sea
TypeGulf
OutflowRed Sea
Basin countriesEgypt
Length314 km
Width32 km
Area18000 km2
Depth40 m
Max-depth70 m
CitiesSuez, Ain Sukhna, Ras Gharib

Gulf of Suez. The Gulf of Suez is a northwestern arm of the Red Sea, lying entirely within the territory of Egypt and separating the Sinai Peninsula from the mainland of Africa. It is a vital maritime corridor, historically significant for trade and, in the modern era, critically important for its substantial petroleum reserves. The gulf extends approximately 314 kilometers from its head at the city of Suez to its mouth at the Strait of Gubal, where it meets the main body of the Red Sea.

Geography

The Gulf of Suez is a relatively shallow, elongated basin, bordered to the east by the mountainous terrain of the Sinai Peninsula and to the west by the arid Eastern Desert of the African continent. Major ports and settlements along its coast include the city of Suez at its northern terminus, the industrial port of Ain Sukhna, and the oil-exporting town of Ras Gharib. The southern entrance to the gulf is marked by the Strait of Gubal, which opens into the Red Sea proper near the resort city of Hurghada. Its coastline features a mix of sandy beaches, coral reefs, and extensive coastal lagoons, such as those near the Suez Canal entrance.

Geology

Geologically, the Gulf of Suez forms the northern part of the Red Sea Rift, a divergent tectonic boundary between the African Plate and the Arabian Plate. It is considered a continental rift, an early-stage ocean basin that has not yet developed a full mid-ocean ridge. The region is seismically active, with numerous fault lines, such as the Clysmic Fault, running parallel to its axis. This extensional tectonics has created a series of deep sedimentary basins, including the Belayim Marine and October Field areas, which are filled with thick sequences of Miocene and Pliocene strata that form the primary reservoirs for the region's hydrocarbons.

Ecology

The marine environment of the Gulf of Suez hosts diverse ecosystems, though it faces significant environmental pressures. Its waters contain extensive coral reef formations, particularly in the southern reaches near the Strait of Gubal, which are part of the larger Red Sea reef system. These reefs support a variety of marine life, including populations of the dugong, as well as numerous species of fish, crustaceans, and mollusks. The northern, more industrialized end of the gulf is subject to pollution from shipping traffic associated with the Suez Canal and offshore oil platforms, impacting local mangrove stands and seagrass beds.

Economic importance

The Gulf of Suez is one of Egypt's most critical economic regions due to its vast petroleum and natural gas resources. Major offshore oil fields, such as the Morgan Field and the Ras Budran field, have been in production for decades under the operations of companies like the Gulf of Suez Petroleum Company and Petroleum Projects and Technical Consultations Company. The gulf also serves as a key shipping lane for tankers exiting the Suez Canal, heading to markets in Europe and the Americas. Additionally, the coasts support industries like salt production and tourism, with resorts in Ain Sukhna and diving centers near Hurghada.

History

The gulf has been a conduit for trade and naval power for millennia, connecting Ancient Egypt with the land of Punt. In the 19th century, it gained global strategic prominence with the construction of the Suez Canal, engineered by Ferdinand de Lesseps and opened in 1869, which linked it directly to the Mediterranean Sea. The region was a focal point during the Suez Crisis of 1956, involving Israel, France, and the United Kingdom, and again during the Arab-Israeli conflict, notably the War of Attrition and the Yom Kippur War in 1973. The Camp David Accords later demilitarized the Sinai Peninsula, stabilizing the area.

Category:Gulfs of the Red Sea Category:Geography of Egypt Category:Rift valleys