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At the mid-ocean ridges, new ocean floor is continuously being created from rising magma originating from the Earth's mantle. The creation of the new oceanic crust pushes older crust away from the ridge in a conveyor belt fashion. This process is known as sea-floor spreading. The fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies. A narrow depressed area running along the center of the ridges, called a rift, is the region where volcanic activity is adding magma to the two diverging pieces of oceanic crust.

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Related Questions

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