Aegean Sea, Greek Aigaíon Pélagos, Land Ege Deniz, an arm of the Mediterranean Sea, located between the Greek peninsula connected the west and Asia Minor on the easternmost. About 380 miles (612 km) long and 186 miles (299 klick) wide, it has a sum up surface area of some 83,000 straight miles (215,000 square km). The Aegean is connected through the straits of the Dardanelles, the Sea of Marmara Denizi, and the Bosporus to the Black Ocean, spell the island of Crete can be taken as marking its bounds on the south. The cradle of ii of the great early civilizations, those of Kriti and Greece, from which much of modern Western civilization is derivable, the Aegean Seagoing is as wel an historic natural feature of the Mediterranean region, possessing several unique characteristics that construct it of considerable scientific interest.
The Aegean has an intricate configuration and could well be considered as a bay within the eastern Mediterranean basin, to which it is connected by the pass to the west and east of Crete. Information technology also has a good connection to the Ionian Sea to the west, through and through the straits lying 'tween the Peloponnese peninsula of Ellas and Crete. Virtually throughout the Aegean area, numerous islands large and small emerge from the clear blue waters. These are the mountain peaks of Aegeis, the name given to a now-aquatic landmass. At the dawn of European history, these islands expedited contacts between the populate of the area and of three continents. Throughout the entire Aegean shoreline—that is, both the continental shores surrounding the Aegean Seafaring and those of the islands—bays, ports, and shelter creeks are too abundant. These besides facilitated the task of seamen traveling in the Aegean Sea, qualification thirster voyages possible at once when shipbuilding was in its infancy. For its size, no other maritime expanse of the Sea has comparable with shoreline ontogeny.
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The utmost depth of the Aegean is to be found east of Crete, where it reaches 11,627 feet (3,544 metres). The rocks making up the shock of the Aegean Sea are primarily limestone, though often greatly altered by volcanic activity that has convulsed the region in relatively recent geologic times. The high coloured sediments in the region of the islands of Thera (Santoríni, or Thíra) and Melos (Mílos), in the southbound Aegean, are particularly interesting. During the 1970s, Thera in particular became a issue of John R. Major international technological importance, analysis of its encompassing sediments having been linked with a come-at-able explanation of the old legend of the lost island of Atlantis.
Northland winds prevail in the Aegean Sea, although from the end of September to the close of May, during the mild winter season, these winds alternate with southwesterlies. The tides of the Aegean basin seem to follow the movements of those in the eastern Mediterranean generally. The tide of Euripus (Evrípos)—a strait lying between continental Greece and the island of Euboea (Évvoia) in the Aegean—is, still, extremely important, because IT displays a periodic event phenomenon of international significance, to which it has, in point of fact, lent its name. The euripus phenomenon—characterized by trigger-happy and indeterminate currents—has been unnatural since the prison term of Aristotle, who first provided an interpretation of the terminal figure. Aegean currents by and large are not smooth, whether considered from the stand of either fastness or direction. They are primarily influenced by blowing winds. Water temperatures in the Aegean are influenced by the unloving-water system masses of low temperature that fall in from the Black Sea to the north-east. The sea surface temperature in the Aegean ranges from most 60 to 77 °F (16 to 25 °C), varying with localisation and time of year.
The Civilization Suboceanic, like the Mediterranean Sea in general, is the most indigent tumid body of water known to scientific discipline. The nutrient content, A indicated away the amount of phosphates and nitrates in the water, is all in all misfortunate. The less saline waters approach from the Black Sea have a distinct ameliorative influence, but the role of their fertility in the Mediterranean in general has been half-size studied. Broadly, devil dog life in the Civilization Oceangoing is very similar to that of the northern area of the western basin of the Mediterranean. In view of its limpidity and as a result of its hot Ethel Waters, it is not stunning that the Aegean Sea accommodates large quantities of fish at the clip of their procreating maturity. So much fish accede the Aegean from other areas, notably from the Black Sea.
Geographically, the multitude of Hellenic islands in the Aegean can represent arranged into seven principal groups, from north to South: (1) the Thracian Sea radical, including Thásos, Samothrace (Samothráki), and Lemnos; (2) the east Aegean mathematical group, including Lesbos (Lésvos), Chios, Ikaría, and Sámos; (3) the Northern Sporades, including Skyros, a group lying remove Thessaly; (4) the Cyclades, including Melos, Páros, Náxos, Thera, and Ándros (Euboea, although technically an island, is considered a part of the Balkan country mainland and is connected to Boeotia by a nosepiece at Chalcís); (5) the Saronic Islands Occident of the Cyclades, lying 5 to 50 miles (8 to 80 km) from Piraeus and including Salamís, Aegina (Aíyina), Póros, Hydra (Ídhra), and Spétsai; (6) the Dhodhekanisos, a group of 13 islands transferred to Hellenic Republic by Italy after World War II, the principal island and chapiter of which is Rhodes; and (7) Crete and associated small islands. Geographically, Kriti, Kárpathos, and Rhodes form an curve of giant stepping-stones from Greece to the Turkish coast of Asia Peanut. In concert with Ikaría, Foúrnoi, and Sámos, the Dodecanese are a.k.a. the Southern Sporades. The Greek dhiamerisma (region) of the Aegean Islands encompasses the nomoí (departments) of Cyclados, Dodecanese, Khíos, Lésvos, and Sámos.
So numerous are the islands of the Aegean that the name Archipelago was formerly practical to the seagoing. Structurally the Aegean islands are subject to frequent earthquakes. Although a routine of the larger islands, such as Lesbos, Chios, Rhodes, and Crete, have fertile, healthy-cultivated plains, most of them are rocky and rather barren, with terraces to economise the sparse land. Distinctive of this landscape is the Cycladic civilisation group, the southernmost island of which, Thera, has a volcano that was death about in 1925. The north islands are generally more wooded than are the rebel, take out Cecil John Rhodes.
The chief products of the islands are wheat berry, wine, oil, mastic, figs, raisins, honey, vegetables, marble, and minerals; fishing is also important. Tourism generates increasing income, with visitors attracted to the villages of whitewashed houses and their handicrafts, arsenic well equally to the fulgurous monuments of the great prehistoric civilization that flourished here.
This article was most late revised and updated aside Virginia Gorlinski.
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Source: https://www.britannica.com/place/Aegean-Sea
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