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Mediterranean Sea. The Mediterranean Sea is the body of water that separates Europe, Africa, and Asia . The Mediterranean Sea is connected to the Atlantic Ocean by a narrow passage called the Strait of Gibraltar. The sea is almost completely surrounded by land, on the north by Europe, on the south by North Africa, and on the east by the Middle ...
The Mediterranean Sea ( / ˌmɛdɪtəˈreɪniən / MED-ih-tə-RAY-nee-ən) is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant in West Asia. The Mediterranean has played a ...
- 1,500 m (4,900 ft)
- 2,500,000 km² (970,000 sq mi)
- 5,109 m (16,762 ft) ±1 m (3 ft)
- 3,750,000 km³ (900,000 cu mi)
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A mediterranean sea ( / ˌmɛdɪtəˈreɪniən / MED-i-tə-RAY-nee-ən) is, in oceanography, a mostly enclosed sea that has limited exchange of water with outer oceans and whose water circulation is dominated by salinity and temperature differences rather than by winds or tides. [1] [2] The eponymous Mediterranean Sea, for example, is almost ...
Mediterranean region. The Mediterranean region is the region surrounding the Mediterranean Sea. This includes places from Europe and Africa and Asia. Most of the region has a Mediterranean climate with warm to hot dry summers and cool to mild wet winters. Plants that grow there are short trees and shrubs which survive the yearly drought during ...
Simple machine. The six classical simple machines. A simple machine is a mechanical device that changes the direction or magnitude of a force. [1] In general, they can be defined as the simplest mechanisms that use mechanical advantage (also called leverage) to multiply force. [2] Usually the term refers to the six classical simple machines ...
Afrikaans; Alemannisch; Anarâškielâ; العربية; Asturianu; Azərbaycanca; تۆرکجه; বাংলা; Башҡортса; Беларуская ...
The temperature of the sea depends on the amount of sunlight falling on the surface. In the tropic s, with the sun nearly overhead, the temperature of the surface layers can rise to over 30 °C (86 °F). Near the poles the temperature in balance with the sea ice is about −2 °C (28 °F). Cold water is denser than warm water and tends to sink.
