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At mid-oceanic ridges, plates are pulled apart in two separate directions. This creates a gap (rift valley), allowing for warm, buoyant magma to rise to the surface and cool. As the magma cools, it creates ridges along the rift valleys. The elevation is caused by the excess amount of newly created, less dense oceanic crust. This crust occupies more volume, which causes it to be higher up than the surrounding, older crust.

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โˆ™ 2009-03-17 03:57:27
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Earthquakes

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Q: What type of magmatic activity is characteristic of mid oceanic ridges?
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