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An oceanic ridge is an underwater mountain range, usually
formed by plate tectonics.
They are geologically active, with new magma constantly emerging onto the ocean floor through a gap called a rift in the
earth's crust. In most instances, it accumulates and forms new crust. However, submarine volcanoes might also be formed.
The rocks making up the sea floor are usually younger near the centre of the ridge and the older ones located farther away
from the rift. This is evidence that new magma constantly emerges through a rift.
Also, the sea floor is made up of rocks generally much younger than the Earth itself. This suggests that the sea floor is in a
constant state of 'renewal'.
- Atlantic-Indian
Ridge
- East Pacific
Rise
- Emperor Seamounts
- Explorer Ridge
- Gakkel Ridge
- Gorda Ridge
- Hawaiian Ridge
- Juan de Fuca
Ridge
- Kerguelen
Plateau
- Mid-Atlantic Ridge
- Mid-Indian Ridge
- Nazca Ridge
- Pacific-Antarctic Ridge
- Reykjanes Ridge
- Bermuda Rise
- Rockall Rise
- Southeast
Indian Rise
- Southwest
Indian Ridge
- Walvis Ridge
See also: Oceanic trench, plate tectonics, earth science, list of landforms.
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