An ocean is a continuous body of salt water that surrounds the continents and fills the Earth's great depressions. The ocean's cover about 71% of the Earth's surface (more than 80% of the Southern Hemisphere) and comprise about 98% of the water of the planet.
There are five main oceans: the Atlantic, Pacific, Indian, Arctic, and Antarctic. They may be described by distinct region (littoral, benthos, pelagic, and abyssal), or by depth (continental shelf or margin, deep sea plain, and ocean trench). The seafloor has a varied topography. See also mid-ocean ridge.
Seawater contains salt and other mineral deposits; the salt content, between 3.3% and 3.7%, is the result of washout from the land and interchange with the atmosphere over the ages. Light penetrates seawater to a maximum depth of about 300 meters (1,000 feet), below which plant life cannot grow.
History of the oceansThrough volcanic activity the oceans have been forming over the last 200 million years. The theory of continental drift (and associated seafloor spreading) has revealed that the ancient supercontinent Pangea was surrounded by a vast ocean, Panthallasia. As Pangaea began to split, a smaller and shallower ocean, the Tethys Sea, formed between the continents. By about 65 million years ago, the Atlantic and Indian oceans appeared. The Pacific became separated from the Atlantic and Indian oceans when the North and South American continents joined. The separation of Greenland from North America, and the widening of the North Atlantic, completed the encirclement of the Arctic Ocean. See also origin of the oceans.
Related category GEOGRAPHY
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