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Straits of Gibraltar

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Straits of Gibraltar

The Strait of Gibraltar (Arabic: مضيق جبل طارق, Spanish: Estrecho de Gibraltar) is a narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates Gibraltar and Spain in Europe from Morocco in Africa. The name comes from the Rock of Gibraltar, which in turn originates from the Arabic Jebel Tariq (meaning "Tariq's mountain"[1]) named after Tariq ibn Ziyad. It is also known as the Straits of Gibraltar, or STROG (Strait Of Gibraltar), in naval use[2] and as the "Pillars of Hercules" (Ancient Greek: αἱ Ἡράκλειοι στῆλαι)[3] in the ancient world.

Europe and Africa are separated by 7.7 nautical miles (14.3 km; 8.9 mi) of ocean at the strait's narrowest point. The Strait's depth ranges between 300 and 900 metres (160 and 490 fathoms; 980 and 2,950 ft)[4] which possibly interacted with the lower mean sea level of the last major glaciation 20,000 years ago[5] when the level of the sea is believed to have been lower by 110–120 m (60–66 fathoms; 360–390 ft).[6] Ferries cross between the two continents every day in as little as 35 minutes. The Spanish side of the Strait is protected under El Estrecho Natural Park.

Location

On the northern side of the Strait are Spain and Gibraltar (a British overseas territory in the Iberian Peninsula), while on the southern side are Morocco and Ceuta (a Spanish exclave in North Africa). Its boundaries were known in antiquity as the Pillars of Hercules. There are several islets, such as the disputed Isla Perejil, that are claimed by both Morocco and Spain.[7]

Due to its location, the Strait is commonly used for illegal immigration from Africa to Europe.[8]

Extent

The International Hydrographic Organization defines the limits of the Strait of Gibraltar as follows:[9]

On the West. A line joining Cape Trafalgar to Cape Spartel.
On the East. A line joining Europa Point to P. Almina (35°54′N 5°18′W / 35.900°N 5.300°W / 35.900; -5.300).

Geology

Around 5.9 million years ago,[10] the connection between the Mediterranean Sea and the Atlantic Ocean along the Betic and Rifan Corridor was progressively restricted until its total closure, effectively causing the salinity of the Mediterranean to periodically fall within the gypsum and salt deposition range, during what is known as the Messinian Salinity Crisis. In this water chemistry environment, dissolved mineral concentrations, temperature and stilled water currents combined properly and occurred regularly to precipitate many mineral salts in sea floor bedded layers. The resultant accumulation of various huge salt and mineral deposits about the Mediterranean basin are directly linked to this era. It is believed that this process took a short time, by geological standards, lasting between 500,000 and 600,000 years.

It is estimated that, were the straits closed even at today's higher sea level, most water in the Mediterranean basin would evaporate within only a thousand years, as it is believed to have done then,[10] and such an event would lay down similar mineral deposits as those such as the salt mines now found under the sea floor all over the Mediterranean.

After a lengthy period of restricted intermittent or no water exchange between the Atlantic Ocean and Mediterranean basin, approximately 5.33 million years ago,[11] the Atlantic-Mediterranean connection was completely reestablished through the Strait of Gibraltar by the Zanclean flood, and has remained open ever since.[12] The erosion produced by the incoming waters seem to be the main cause for the present depth of the strait (900 m at the narrows, 280 m at the Camarinal Sill). The strait is expected to close again as the African Plate moves northward relative to the Eurasian Plate, but on geological rather than human timescales.

Important Bird Area

The Strait has been identified as an Important Bird Area by BirdLife International because hundreds of thousands of seabirds use it every year to pass between the Mediterranean and the Atlantic, including large numbers of Cory's and Balearic Shearwaters, Audouin's, Yellow-legged and Lesser Black-backed Gulls, Razorbills and Atlantic Puffins.[13]

History

For full articles on the history of the north Gibraltar shore, see History of Gibraltar or History of Spain. For the full article on the history of the south Gibraltar shore, see History of Morocco.

Evidence of the first human habitation of the area by Neanderthals dates back to 125,000 years ago. In fact, it is believed that the Rock of Gibraltar may have been one of the last outposts of Neanderthal habitation in the world, with evidence of their presence there dating to as recently as only 24,000 years ago.[14] Archaeological evidence of Homo sapiens habitation of the area dates back to ca. 40,000 years ago.

Beginning in 1492, the straits began to play a certain cultural role in acting as a barrier against cross-strait conquest and the flow of culture and language that would naturally follow such a conquest. In that year, the last Muslim government north of the straits was overthrown by a Spanish force. Since that time, the straits have come to foster the development of two very distinct and varied cultures on either side of the straits.

On the northern side, the Christian/European culture has remained dominant (as it used to be in the southern side too), along with the Latin-based Spanish language, while on the southern side, the markedly different Muslim-Arabic/Mediterranean culture came to dominate later, along with the Arabic language. For the last 500 years, religious and cultural intolerance, more than the small travel barrier that the straits present, has come to act as a powerful enforcing agent of the cultural separation that exists between these two groups.

The small British enclave of the city of Gibraltar presents a third cultural group found in the straits. This enclave was first established in 1704 and has since been used by Britain to act as a surety for control of the sea lanes into and out of the Mediterranean.

Following the Spanish coup of July 1936 the Spanish Republican Navy tried to blockade the Strait of Gibraltar to hamper the transport of Army of Africa troops from Spanish Morocco to Peninsular Spain. But on 5 August 1936 the so-called Convoy de la victoria was able to bring at least 2,500 men across the strait breaking the republican blockade.[15]

Communications


The Strait is an important shipping route from the Mediterranean to the Atlantic. There are ferries that operate between Spain and Morocco across the strait, as well as between Spain and Ceuta and Gibraltar to Tangier.

Tunnel across the strait

Main article: Gibraltar Tunnel

In December 2003, Spain and Morocco agreed to explore the construction of an undersea rail tunnel to connect their rail systems across the Strait. The gauge of the rail would be 1,435 mm (4 ft 8.5 in) to match the proposed construction and conversion of significant parts of the existing broad gauge system to standard gauge.[16] While the project remains in a planning phase, Spanish and Moroccan officials have met to discuss it as recently as 2012,[17] and proposals predict it could be completed by 2025.

Special flow and wave patterns

The Strait of Gibraltar links the Atlantic Ocean directly to the Mediterranean Sea. This direct linkage creates certain unique flow and wave patterns. These unique patterns are created due to the interaction of various regional and global evaporative forces, tidal forces, and wind forces.

Inflow and outflow


Through the strait, water generally flows more or less continually in both an eastward and a westward direction. A smaller amount of deeper saltier and therefore denser waters continually work their way westwards (the Mediterranean outflow), while a larger amount of surface waters with lower salinity and density continually work their way eastwards (the Mediterranean inflow). These general flow tendencies may be occasionally interrupted for brief periods to accommodate temporary tidal flow requirements, depending on various lunar and solar alignments. Still, on the whole and over time, the balance of the water flow is eastwards, due to an evaporation rate within the Mediterranean basin higher than the combined inflow of all the rivers that empty into it. The shallow Camarinal Sill of the Strait of Gibraltar, which forms the shallowest point within the strait, acts to limit mixing between the cold, less saline Atlantic water and the warm Mediterranean waters. The Camarinal Sill is located at the far western end of the strait.

The Mediterranean waters are so much saltier than the Atlantic waters that they sink below the constantly incoming water and form a highly saline (thermohaline, both warm and salty) layer of bottom water. This layer of bottom-water constantly works its way out into the Atlantic as the Mediterranean outflow. On the Atlantic side of the strait, a density boundary separates the Mediterranean outflow waters from the rest at about 100 m (330 ft) depth. These waters flow out and down the continental slope, losing salinity, until they begin to mix and equilibrate more rapidly, much further out at a depth of about 1,000 m (3,300 ft). The Mediterranean outflow water layer can be traced for thousands of kilometres west of the strait, before completely losing its identity.

During the Second World War, German U-boats used the currents to pass into the Mediterranean Sea without detection, by maintaining silence with engines off.[18] From September 1941 to May 1944 Germany managed to send 62 U-boats into the Mediterranean. All these boats had to navigate the British-controlled Strait of Gibraltar where nine U-boats were sunk while attempting passage and 10 more had to break off their run due to damage. No U-boats ever made it back into the Atlantic and all were either sunk in battle or scuttled by their own crews.[19]

Internal waves

Internal waves (waves at the density boundary layer) are often produced by the strait. Like traffic merging on a highway, the water flow is constricted in both directions because it must pass over the Camarinal Sill. When large tidal flows enter the Strait and the high tide relaxes, internal waves are generated at the Camarinal Sill and proceed eastwards. Even though the waves may occur down to great depths, occasionally the waves are almost imperceptible at the surface, at other times they can be seen clearly in satellite imagery. These internal waves continue to flow eastward and to refract around coastal features. They can sometimes be traced for as much as 100 km (62 mi), and sometimes create interference patterns with refracted waves.[20]

Power generation

Some studies have proposed the possibility of erecting tidal power generating stations within the strait, to be powered from the predictable current at the strait.

In the 1920s and 1930s, the Atlantropa project proposed damming the strait to generate large amounts of electricity and lower the sea level of the Mediterranean by several hundreds of meters to create large new lands for settlement.[21]

See also

References and notes

External links

  • http://www.agu.org/sci_soc/eosrjohnsonf3.gif Building the dam and letting the Mediterranean Sea completely evaporate would raise Sea Level 15 meters over 1,000 years. Evaporating the first 100 meters or so would raise Sea Level 1 meter in about 100 years.
  • Project for a Europe-Africa permanent link through the Strait of Gibraltar — United Nations Economic and Social Council, 2001. Accessed 26 February 2006.
  • (Spanish) Estudios Geográficos del Estrecho de Gibraltar — La Universidad de Tetuán and La Universidad de Sevilla. Accessed 26 February 2006.

Coordinates: 35°58′18″N 5°29′09″W / 35.97167°N 5.48583°W / 35.97167; -5.48583

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