| Strait Of Gibraltar |
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The Strait of Gibraltar ( use.See, for instance, Nato Medals: Medal for Active Endeavor , awarded for activity in the international water of the Mediterranean and STROG. There are 8 miles (13 km) of ocean separating Europe from Africa at the strait's narrowest point. The strait depth ranges between 300 and 900 meters.See Robinson, Allan Richard and Paola Malanotte-Rizzoli, ''Ocean Processes in Climate Dynamics: Global and Mediterranean Examples''. Springer, 1994, p. 307, ISBN ISBN 0792326245. LOCATION On the northern side of the Strait is Spain and Gibraltar , while on the southern side is Morocco and Ceuta , a Spanish Exclave in North Africa . Its boundaries were known in antiquity as the Pillars Of Hercules . There are several small islands, such as the Disputed Isla Perejil , that are claimed by both Spain and Morocco.Tremlett, Giles, "Moroccans seize Parsley Island and leave a bitter taste in Spanish mouths," in '' The Guardian '', July 13, 2002. GEOLOGY About 6 million years ago, the Strait closed, effectively turning the Mediterranean into a huge salty lake that eventually dried up, in what is known as the Messinian Salinity Crisis . The Mediterranean then turned into a lake, known as the Mediterranean Sea . At the Miocene / Pliocene boundary, approximately 5.33 million years ago, the Strait opened up for the last time, and has remained open since. Cloud, P. , ''Oasis in space. Earth history from the beginning'', New York: W.W. Norton & Co. Inc., p. 440. ISBN 0393019527 COMMUNICATIONS The Straits are 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 Tunnel across the strait See Also: Gibraltar Tunnel In December 2003, Spain and Morocco agreed to explore the construction of an INFLOW AND OUTFLOW s (marked with arrows) caused by the Strait of Gibraltar]] On a net basis, water continually flows eastward into and through the Strait of Gibraltar, due to an evaporation rate within the Mediterranean basin higher than the combined inflow of all the rivers that empty into it. The Sill of the Strait of Gibraltar acts to limit mixing between the cold, less saline Atlantic water and the warm Mediterranean waters. The latter are so much saltier that they sink below the constantly incoming Atlantic water and form a highly saline ('' Thermohaline '', both warm and salty) bottom water, called the Mediterranean Outflow . A density boundary separates the layers at about 100 m depth. It flows out and down the continental slope, losing salinity, until it equilibrates after mixing at a depth of about 1000 meters. The Mediterranean outflow water can be traced for thousands of kilometers before losing its identity. Internal Wave s (waves at the density boundary layer) are common in the strait. Like traffic merging on a highway, the water flow is constricted in both directions because it must pass over a shallow submarine barrier, the Camarinal Sill . When large tidal flows enter the Strait, internal waves are set off at the Camarinal Sill as the high tide relaxes. The waves—sometimes with heights up to 100 m—travel eastward. Even though the waves occur at great depth and the height of the waves at the surface is almost nothing, they can be traced in the Sunglint because they concentrate the biological films on the water surface, creating slight differences in roughness. The waves flow eastward, refract around coastal features; can be traced for as much as 150 km, and sometimes create Interference Pattern s with refracted waves.Wesson, J.C. and M.C. Gregg, "Mixing at Camarinal Sill in the Strait of Gibraltar," in ''Journal of Geophysical Research'', Vol. 99, No. C5, 1994, pp.9847–9878. SEE ALSO EXTERNAL LINKS
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