Mediterranean Sea

"Mediterranean" redirects here.

Composite satellite image of the Mediterranean Sea.

A point between Minorca and Barcelona

The Mediterranean Sea (35 degrees north, 18 degrees east) is a sea of the Atlantic Ocean almost completely enclosed by land: on the north by Europe, on the south by Africa, and on the east by Asia. It covers an approximate area of 965,000 square miles (2.5 million km²), but its connection to the Atlantic (the Strait of Gibraltar) is only eight miles (13 km) wide. In oceanography, it is sometimes called the Eurafrican Mediterranean Sea or the European Mediterranean Sea, to distinguish it from mediterranean seas elsewhere.

The western extremity of the Mediterranean connects with the Atlantic Ocean by the narrow and shallow channel of the Strait of Gibraltar, which is only eight miles wide at its narrowest point; and the depth of the sill, or submarine ridge separating the Atlantic from the Alborán Sea, is 1,050 feet (320 metres). To the northeast the Mediterranean Sea is connected with the Black Sea through the Dardanelles (with a sill depth of 230 feet), the Sea of Marmara, and the strait of the Bosporus (sill depth of about 300 feet). To the southeast it is connected with the Red Sea by the Suez Canal.

Historically, the Mediterranean has provided a way of life for many societies around its borders. It was the most important route for merchants and travelers of ancient times, allowing for trade and cultural exchange between emergent peoples of the region — the Mesopotamian, Egyptian, Semitic, Persian, Phoenician, Carthaginian, Greek and Roman cultures. Knowledge of the history of the Mediterranean is crucial to understanding the origins and development of many modern societies. In the past few centuries, human activity has brought about irreversible changes in the ecology and geology of the Mediterranean Sea.

Name

The term Mediterranean derives from the Latin mediterraneus, 'inland' (medius, 'middle' + terra, 'land, earth'). To the ancient Romans, the Mediterranean was the center of the Earth as they knew it.

The Mediterranean Sea has been known by a number of alternative names throughout human history. It was, for example, commonly called Mare Nostrum (Latin, Our Sea), and occasionally Mare Internum by the Romans. (Sallust, Jug. 17). The Greeks name it Mesogeios (Μεσόγειος), meaning inland, interior (μεσο, 'middle' + γαιος, 'land, earth'). In the Old Testament, on the west coast of the Holy Land, and therefore behind a person facing the east, it is called the "Hinder Sea", sometimes translated as "Western Sea", (Deut. xi. 24; Joel, ii. 20), and also the "Sea of the Philistines" (Exod. xxii. 81), because that people occupied a large portion of its shores near the Israelites. Mostly, however, it was the "Great Sea" (Num. xxxiv. 6, 7; Josh. i. 4, ix. 1, xv. 47; Ezek. xlvii. 10, 15, 20), or simply "The Sea" (1 Kings, v. 9; comp. 1 Macc. xiv. 34. xv. 11). In Hebrew, it is called HaYam HaTikhon (הַיָּם הַתִּיכוֹן), "the middle sea", a literal adaptation of the German equivalent Mittelmeer. In Turkish, it is Akdeniz, "the white sea". In Arabic, it is Al-Baħr Al-Abyad Al-Muttawasit (البحر الأبيض المتوسط), "the middle white sea".

History

During ancient times, the Mediterranean Sea was an important route for merchants and travelers, allowing for trade and cultural exchange between emergent peoples of the region — the Mesopotamian, Egyptian, Semitic, Persian, Phoenician, Carthaginian, Greek and Roman cultures. The Mediterranean provided a way of life for many societies around its borders. Knowledge of the history of the Mediterranean is crucial to understanding the origins and development of many modern societies.

Geography and Climate

On the west, The Mediterranean Sea is connected to the Atlantic Ocean by the Strait of Gibraltar, a relatively shallow channel which at its narrowest point is only eight miles (13 km) wide. To the northeast it is linked to the Black Sea, by the Dardanelles and the Bosporus respectively, on the east. The Sea of Marmara is often considered a part of the Mediterranean Sea, whereas the Black Sea is generally not. The man-made Suez Canal in the southeast connects the Mediterranean Sea with the Red Sea.

Large islands in the Mediterranean include Cyprus, Crete, Euboea, Rhodes, Lesbos, Chios, Kefalonia and Corfu in the eastern Mediterranean; Sardinia, Corsica, Sicily, and Malta in the central Mediterranean; and Ibiza, Majorca and Minorca (the Balearic Islands) in the western Mediterranean.

The Mediterranean climate is generally one of wet winters and hot, dry summers. Crops of the region include olives, grapes, oranges, tangerines, and cork.

Oceanography

The character of the Mediterranean Sea is determined by the fact that it is nearly landlocked. As a result of the narrow connection with the Atlantic Ocean, tides are very limited. The Mediterranean is characterized by its imposing deep blue color, especially around the Greek islands.

Salinity and Currents

Predominant currents for June

Evaporation greatly exceeds precipitation and river runoff in the Mediterranean, affecting the water circulation within the basin. The quantity of fresh water flowing into the Mediterranean from rivers is only one-third of the amount lost through evaporation. Evaporation is especially high in its eastern half, causing the water level to decrease and salinity to increase eastward. This imbalance causes a pressure gradient which draws relatively cool, low-salinity water from the Atlantic across the basin; it warms and becomes saltier as it travels east, then sinks in the region of the Levant and circulates westward, to spill over the Strait of Gibraltar. Thus, seawater flow is eastward in the Strait's surface waters, and westward below; once in the open ocean, this chemically-distinct "Mediterranean Intermediate Water" can persist thousands of kilometers away from its source.

Salinity in the surface waters of the Mediterranean is about 38 parts per thousand, except in the area closest to the Atlantic, and approaches 40 parts per thousand in the eastern Mediterranean during the summer. Salinity of the deep water is about 38.4 parts per thousand.

The Mediterranean has three layers of water masses; a surface layer, an intermediate layer, and a deep layer that sinks to the bottom. Measurements of the rate at which the deep layer forms and sinks, and studies of heat and water exchange in the Mediterranean provide useful models for understanding the impact of global climactic change on the world’s oceans. Water on the surface of the Mediterranean circulates in separate counterclockwise movements in each of the two basins. The complexity of the northern coastline and the numerous islands cause many eddies and local currents. Tides, although their range is significant only in the Gulf of Gabes and the northern Adriatic, complicate the currents in narrow channels such as the Strait of Messina.

Water Temperature

Areas of the Mediterranean closer to the Equator are hotter in temperature. The Gulf of Sidra, off the coast of Libya, has the highest water temperatures of about 88° F (31° C)in August, followed by the Gulf of Iskenderun with 86° F (30° C). The extreme north of the Adriatic has the lowest surface temperatures; the mean temperature in February falls to 41° F (5° C) in the Gulf of Trieste, and ice occasionally forms in winter.

Bordering Countries

A satellite image taken from the side of the Strait of Gibraltar. At right, Africa; at left, Europe

Twenty-one modern states have a coastline on the Mediterranean Sea. They are:

• Europe (from west to east): Spain, France, Monaco, Italy, the island state of Malta, Slovenia, Croatia, Bosnia and Herzegovina, Montenegro, Albania, Greece
• Asia (from north to south): Turkey, Syria, the island Republic of Cyprus, Lebanon and Israel
• Africa (from east to west): Egypt, Libya, Tunisia, Algeria and Morocco

Mediterranian coast in Israel

Several other territories also border the Mediterranean Sea (from west to east):

• The Crown colony of Gibraltar
• The Spanish exclaves of Ceuta and Melilla and nearby islands
• The autonomous monastic state of Mount Athos
• The sovereign base area of Akrotiri and Dhekelia
• The Gaza Strip (governed by the Palestinian National Authority)

FYROMacedonia, Portugal, San Marino, Serbia, and the Vatican City, although they do not border the sea, are often considered Mediterranean countries in a wider sense due to their Mediterranean climate, fauna and flora, and their cultural affinity with other Mediterranean countries.

Subdivisions

A view across the straits of Gibraltar

The Mediterranean Sea is sub-divided into a number of smaller seas, each with their own designation (from west to east):

• the Alboran Sea, between Spain and Morocco,
• the Balearic Sea, between mainland Spain and its Balearic Islands,
• the Ligurian Sea between Corsica and Liguria (Italy),
• the Tyrrhenian Sea enclosed by Sardinia, Italian peninsula and Sicily,
• the Adriatic Sea between the Italian peninsula and the coasts of Slovenia, Croatia, Bosnia, Montenegro and Albania
• the Ionian Sea between Italy, Greece, and Albania,
• the Aegean Sea between Greece and Turkey, with
  • the Thracian Sea in its north,
  • the Myrtoan Sea between the Cyclades and the Peloponnesos,
  • the Sea of Crete north of Crete
  • the Libyan Sea south of Crete, between the island and Libya
• the Sea of Marmara between the Aegean and Black Seas.
• the Cilician Sea between Turkey and Cyprus

Many of these smaller seas feature in local myth and folklore and derive their names from these associations. In addition to the seas, a number of gulfs and straits are also recognized:

• the Saint George Bay in Beirut, Lebanon
• the Gulf of Corinth, an enclosed sea between the Ionian Sea and the Corinth Canal
• the Saronic Gulf, the gulf of Athens, between the Corinth Canal and the Mirtoan Sea
• the Thermaic Gulf, the gulf of Thessaloniki, located in the northern Greek region of Macedonia
• the Kvarner Gulf, Croatia
• the Gulf of Lion, south of France
• the Gulf of Valencia, east of Spain.
• the Strait of Messina, between Sicily and the toe of Italy
• the Gulf of Taranto, southern Italy,
• the Strait of Otranto, between Italy and Albania
• the Gulf of Haifa, between Haifa and Akko, Israel
• the Gulf of Sidra, between Tunisia and Cyrenaica (eastern Libya)
• the Strait of Sicily, between Sicily and Tunisia
• the Corsica Channel, between Corsica and Italy
• the Strait of Bonifacio, between Sardinia and Corsica
• the Gulf of İskenderun, between İskenderun and Adana (Turkey)
• the Gulf of Antalya, between west and east shores of Antalya (Turkey)
• the Gulf of Kotor, on the coast of Montenegro

Geology

The geology of the Mediterranean is complex, involving the break-up and then collision of the African and Eurasian plates, and the Messinian Salinity Crisis in the late Miocene when the Mediterranean dried up.

The Mediterranean Sea has an average depth of 1,500 m and the deepest recorded point is 5,267 meters (about 3.27 miles, or 17,200 feet) in the Calypso Deep in the Ionian Sea. The coastline extends for 46,000 km. A shallow submarine ridge (the Strait of Sicily) between the island of Sicily and the coast of Tunisia divides the sea in two main subregions (which in turn are divided into subdivisions), the Western Mediterranean and the Eastern Mediterranean. The Western Mediterranean covers an area of about 0.85 million km² and the Eastern Mediterranean about 1.65 million km². The western section has three submarine basins, the Alborán, the Algerian, and the Tyrrhenian basins (from west to east), divided from one another by submerged ridges. The eastern section is made up of the Ionian Basin (northwest of which is the Adriatic Sea) and the Levantine Basin (northwest of which is the Aegean Sea).

Geodynamic History

The Mediterranean was once thought to be the remnant of the Tethys Ocean. Studies conducted since the 1970s, however, have suggested that the present Mediterranean seafloor is not part of the older (200 million years) Tethys floor. It is now known to be a structurally younger ocean basin (44 million years) known as Neotethys. Neotethys formed during the Late Triassic and Early Jurassic rifting of the African and Eurasian plates.

The geodynamic evolution of the Mediterranean Sea was driven by the convergence of European and African plates. Geologic data suggests that there are at least six main areas where the Africa and Eurasian plates collide, resulting in volcanism, mountain building, and land submergence. The Mediterranean also hosts wide extensional basins and migrating tectonic arcs, in response to its land-locked configuration.

Eastern Mediterranean: in middle Miocene times, the collision between the Arabian microplate and Eurasia led to the separation between the Tethys and the Indian Ocean. This process brought about profound changes in the oceanic circulation patterns, which shifted global climates towards colder conditions. Over the last twenty million years, the Hellenic Arc, which has a land-locked configuration, underwent a widespread extension. During the Pleistocene, the Hellenic Arc experienced a rapid rotation phase, with a counterclockwise component in its eastern portion and a clockwise trend in the western segment.

Central Mediterranean: over the last thirty million years, trench migration and the opening of back arcs caused the formation of the small oceanic basins of the central Mediterranean. This phase was characterized by the counter-clockwise rotation of the Corsica-Sardinia block, which lasted until the Langhian (ca.16 Ma), and was followed by a slab detachment along the northern African margin. Subsequently, a shift of this active extensional deformation led to the opening of the Tyrrenian basin.

Western Mediterranean: Since the Mesozoic period, during convergence between Africa and Iberia in the western Mediterranean developed the Betic-Rif mountain belts. The tectonic model for its evolution includes rapid movement of the Alboran microplate subduction zone and radial extensional collapse, caused by convective removal of lithospheric mantle. The development of these intramontane Betic and Rif basins led to the onset of two marine gateways which were progressively closed during the late Miocene by an interplay of tectonic and glacio-eustatic processes.

Records of Paleoclimatic Variations

Because of its peculiar latitudinal position and its land-locked configuration, the Mediterranean is especially sensitive to astronomically induced climatic variations, which are well documented in its sedimentary record. During dry periods, eolian dust blown from the Sahara is deposited in the Mediterranean, while deposits of detrital mud washed in by rivers prevail during wet periods. Because of this, geological studies of the layers of rock under the Mediterranean which bear marine sapropel (dark-colored sediments containing organic matter) provide us with high-resolution climatic information for the time periods when those sediments were deposited. These data have been employed in reconstructing astronomically calibrated time scales for the last nine million years of Earth’s history. The exceptional accuracy of these paleoclimatic records has improved our knowledge on the Earth’s orbital variations in the past.

Paleoenvironmental Analysis

Its semi-enclosed configuration makes the oceanic gateways critical in controlling circulation and environmental evolution in the Mediterranean Sea. Water circulation patterns are driven by a number of interactive factors, such as climate and bathymetry, which can lead to precipitation of evaporites. During late Miocene times, a so-called “Messinian Salinity Crisis” (MSC hereafter) occurred, which was triggered by the closure of the Atlantic gateway. Evaporites accumulated in the Red Sea Basin (late Miocene), in the Carpatian foredeep (middle Miocene) and in the whole Mediterranean area (Messinian).

An accurate age estimate of the Messinian Salinity Crisis (5.96 million years ago) has recently been astronomically achieved; furthermore, this event seems to have occurred synchronously. The Messinian Salinity Crisis is presumed to have been triggered by tectonic action; however an astronomical influence (eccentricity) might also have been involved. In the Mediterranean basin, diatomites are regularly found underneath the evaporitic deposits, suggesting a connection between their geneses.

The present-day Atlantic gateway, the Strait of Gibraltar, originated in the early Pliocene. In the past there were two other connections between the Atlantic ocean and the Mediterranean Sea, the Betic Corridor (southern Spain) and the Rifian Corridor (northern Morocco). The former closed during Tortonian times, provoking a “Tortonian Salinity Crisis” long before the before the Messinian Salinity Crisis. The Rifian Corridor closed about 6 million years ago, allowing exchanges of mammal species between Africa and Europe.

Ecology

The drying of the sea during the Messinian Salinity Crisis eliminated most of the marine life of that period, and the current marine biota of the Mediterranean are derived primarily from the Atlantic Ocean. The North Atlantic is considerably colder and more nutrient-rich than the Mediterranean, and the marine life of the Mediterranean has had to adapt to its differing conditions in the five million years since the basin was reflooded.

Threats to the Ecology of the Mediterranean

In the last few centuries, mankind has altered Mediterranean geology by digging canals, re-routing rivers and building structures all along the coastlines, exacerbating and changing erosional patterns. Historically, large seasonal inflows from the Nile, which reduced the salinity of coastal waters, were part of an essential cycle influencing the hydrology and the productivity of the fisheries of the southeastern part of the Mediterranean. The construction of the Aswan High Dam in 1970 put an end to this seasonal fluctuation of the discharge of the Nile water into the Mediterranean.

Mismanagement of beaches and overuse of the sea's natural and marine resources continue to be a problem. Industrial pollution and chemical pollution from boats is another threat. Recently the amount of raw sewage being dumped directly into the Mediterranean every year has reached over one million tons. Many marine species have almost disappeared. The Mediterranean monk seal, has been identified as one of the top ten endangered species in the world.

Migration of Invasive Species

The opening of the Suez Canal in 1869 created the first salt-water passage between the Mediterranean and Red seas. The Red Sea is higher than the Eastern Mediterranean, so the canal serves as a tidal strait that pours Red Sea water into the Mediterranean. The Bitter Lakes, which are hypersaline natural lakes that form part of the canal, blocked the migration of Red Sea species into the Mediterranean for many decades, but as the salinity of the lakes gradually 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. The Red Sea is generally saltier and more nutrient-poor than the Atlantic, so the Red Sea species have advantages over Atlantic species in the salty and nutrient-poor Eastern Mediterranean. Accordingly, Red Sea species invade the Mediterranean biota, and not vice versa; this phenomenon is known as the Lessepsian migration (after Ferdinand de Lesseps, the French engineer) or Erythrean invasion. The construction of the Aswan High Dam across the Nile River in the 1960s reduced the inflow of freshwater and nutrient-rich silt from the Nile into the eastern Mediterranean, making conditions there even more like the Red Sea, and worsening the impact of the invasive species.

Invasive species originated from the Red Sea and introduced into the Mediterranean by the construction of the canal have become a major component of the Mediterranean ecosystem, and have serious impacts on the Mediterranean ecology, endangering many local and endemic Mediterranean species. Up to this day, about 300 species native to the Red Sea have already been identified in the Mediterranean Sea, and there are probably others yet unidentified. In recent years, the Egyptian government's announcement of its intentions to deepen and widen the canal, have raised concerns from marine biologists, fearing that this will worsen the invasion of Red Sea species into the Mediterranean by facilitating the crossing of the canal for additional species.

See also

• Mediterranean Basin
• Mediterranean climate
• Mediterranean diet
• Mediterranean forests, woodlands, and shrub
• Mediterranean Games
• Mediterranean race
• Mediterranean sea (oceanography term)
• Mediterranean Union
• Familial Mediterranean fever
• History of the Mediterranean region
• Holy League (Mediterranean)
• Inland Sea, which is sometimes named after the Japanese Mediterranean Sea
• List of islands in the Mediterranean
• Suez Canal

References

ISBN links support NWE through referral fees

• Gedacht, Daniel C. 2004. Land and resources of ancient Rome. Primary sources of ancient civilizations. New York: PowerKids Press. ISBN: 0823967751 9780823967759 0823989437 9780823989430
• Krasheninnikov, Valeriĭ Arkadevich, and John Kendrick Hall. 2005. Geological framework of the Levant. Jerusalem: Historical Productions-Hall. ISBN: 9657297028 9789657297025 9657297036 9789657297032
• Leier, Manfred. 2001. World atlas of the oceans: with the General bathymetric chart of the oceans (GEBCO) published by the Canadian Hydrographic Service. Buffalo: Firefly Books U.S. ISBN: 1552095851 9781552095850
• Levi, Peter. 1991. Atlas of the Greek world. New York, N.Y.: Facts on File. ISBN: 0871964481 9780871964489
• Norwich, John Julius. 2006. The Middle Sea: a history of the Mediterranean. New York: Doubleday. ISBN: 0385510233 9780385510233
• Norwich, John Julius. 1989. Byzantium. New York: Knopf. ISBN: 0394537785 9780394537788 0394537793 9780394537795 0679416501 9780679416500
• O'Shea, Stephen. 2006. Sea of faith: Islam and Christianity in the medieval Mediterranean world. New York: Walker. ISBN: 0802714986 9780802714985
• Pryor, John H. 1988. Geography, technology, and war: studies in the maritime history of the Mediterranean, 649-1571. Cambridge: Cambridge University Press. ISBN: 0521344247 9780521344241
• Symposium on the Mediterranean Sea, and Daniel J. Stanley. 1973. The Mediterranean Sea; a natural sedimentation laboratory. Stroudsburg, Pa: Dowden, Hutchinson & Ross. ISBN: 0879330104 9780879330101
• Westbrook, Graham K., and T. J. Reston. 2002. The accretionary complex of the Mediteranean Ridge: tectonics, fluid flow and the formation of brine lakes. Marine geology, v.186, no. 1-2. Amsterdam: Elsevier.
• Vita-Finzi, Claudio. 1969. The Mediterranean valleys: geological changes in historical times. London: Cambridge U.P. ISBN: 0521073553 9780521073554

External links

• Greenpeace campaign "Defending Our Mediterranean":Threats, Solutions and Photo Petition
• Planblue - Environment and Development in the Mediterranean Region

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