mid-ocean ridge
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Credit: U.S. Geological Survey
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Alaso known as an oceanic spreading ridge, a fracture zone along the ocean bottom where molten mantle material comes to the surface, thus creating new crust. This fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies.
Related category
GEOLOGY AND PLANETARY SCIENCE
Source: U.S. Geological Survey
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