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oceanic ridge

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oceanic ridge

Continuous, submarine mountain chain extending approximately 50,000 mi (80,000 km) through all the world's oceans, separating them into distinct basins. The main ridge extends down the middle of the Atlantic Ocean, passes between Africa and Antarctica, turns north to the Indian Ocean, then continues between Australia, New Zealand, and Antarctica and across the Pacific basin to the mouth of the Gulf of California. Lateral ridges extend from islands on the axis of the oceanic ridge to coasts of adjacent continents. The oceanic ridge system is the largest feature of the Earth's surface after the continents and the ocean basins themselves; it is explained by the theory of plate tectonics as a boundary between diverging plates where molten rock is brought up from deep beneath the Earth's crust. See also subduction zone.


oceanic ridge [‚ō·shē′an·ik ′rij]
(geology)


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113) Thus, a coastal State can define an oceanic ridge as a ridge that lacks morphological continuity with the continental margin and shares genetic and geological characteristics with the deep sea floor.
2007), the most studied ridge system over the longest period of time is the north-south oceanic ridge in the East Pacific.
A controversy among Church (1977, 1978), Laurent (1978), and Oshin and Crocket (1986) concerning the geodynamic significance of the Thetford Mines ophiolites mirrored the debate in the international community concerning the oceanic ridge versus arc settings of ophiolites.
 
 
 
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