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An
ocean is a major body of
saline water, and a component of the hydrosphere. Approximately 71% of the Earth's
surface (an area of some 361 million square kilometers) is covered by ocean, a
continuous body of water that is customarily divided into several principal oceans and smaller
seas. More than half of this area is over 3,000 meters (9,800 ft) deep. Average oceanic
salinity is around 35
parts per thousand (ppt) (3.5%), and nearly all seawater has a salinity in the range of 30 to 38 ppt. Though generally recognized as several 'separate' oceans, these waters comprise one global, interconnected body of salt water often referred to as the
World Ocean or global ocean.
[6][7] This concept of a global ocean as a continuous body of water with relatively free interchange among its parts is of fundamental importance to
oceanography.
[8] The major oceanic divisions are defined in part by the
continents, various
archipelagos, and other criteria: these divisions are (in descending order of size) the
Pacific Ocean, the
Atlantic Ocean, the
Indian Ocean, the
Southern Ocean and the
Arctic Ocean.
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