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Ophiolites are created under mid-ocean ridges and represent a vertical section beneath a ridge system. One of the best ophiolites is seen in the Troodos range in Southern Cyprus. The topmost layer is invariably pillow lavas which are usually basaltic lavas that were erupted under water.

Then as an ocean closes due to subduction, part of the ocean ridge system MAY be scrapped off and by a process called OBDUCTION be forced onto the plate which is over-riding which is usually the continental plate. If the processes cause the obducted mass to rise above sea level the result is an ophiolite.

So whilst they are created at mid-ocean ridges they are the result of subduction.

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