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The Mediterranean Sea encompasses a vast number of islands, some of them of volcanic origin. The two largest islands, in both area and population, are Sicily and Sardinia. The Mediterranean Sea has an average depth of 1,500 m (4,900 ft) and the deepest recorded point is 5,109 ± 1 m (16,762 ± 3 ft) in the Calypso Deep in the Ionian Sea.
The General Bathymetric Chart of the Oceans (GEBCO) is a publicly available bathymetric chart of the world's oceans. The project was conceived with the aim of preparing a global series of charts showing the general shape of the seafloor. Over the years it has become a reference map of the bathymetry of the world's oceans for scientists and others.
A bathymetric chart is a type of isarithmic map that depicts the submerged bathymetry and physiographic features of ocean and sea bottoms. [1] Their primary purpose is to provide detailed depth contours of ocean topography as well as provide the size, shape and distribution of underwater features.
The first dives of the 2020 season commenced with dives to the French submarine Minerve in the Mediterranean Sea on 1–2 February 2020, and the second crewed descent to the Calypso Deep. [ 2 ] [ 3 ] On 10 February 2020 Victor Vescovo and Prince Albert II of Monaco reached the bottom of the Calypso Deep at a newly calculated depth of 5,109 m ...
The greatest depth of 4,384 m (14,383 ft) is found in the Pliny Trench, about 80 km (50 mi) south of Crete. The Levantine Sea covers 320,000 km 2 (120,000 sq mi). The northern part of the Levantine Sea between Cyprus and Turkey can be further specified as the Cilician Sea, a term more arcane.
The average depth of the oceans is about 4 km. More precisely the average depth is 3,688 meters (12,100 ft). [72] Nearly half of the world's marine waters are over 3,000 meters (9,800 ft) deep. [27] "Deep ocean," which is anything below 200 meters (660 ft), covers about 66% of Earth's surface. [87]
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In oceanography, a mediterranean sea (/ ˌ m ɛ d ɪ t ə ˈ r eɪ n i ə n / MED-ih-tə-RAY-nee-ən) is 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.