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The Cocos Plate is an oceanic tectonic plate beneath the Pacific Ocean off the west coast of Central America. The Cocos Plate is created by sea floor spreading along the East Pacific Rise, specifically in a complicated area geologists call the Cocos-Nazca spreading system. From the rise the plate is pushed eastward and pushed or dragged (perhaps both) under the less dense overriding Caribbean Plate in the process called subduction. The subducted leading edge heats up and adds its water to the mantle above it. In the mantle layer called the aesthenosphere, mantle rock melts to make magma. As a result, to the northeast of the subducting edge is the continuous arc of volcanos stretching from Costa Rica to Guatemala and a belt of earthquakes that extends farther north, into Mexico.
The northeasterly side is a convergent boundary subducting under the North American Plate to the north and the South American Plate to the south. The Cocos Plate is bounded to the south by the Nazca Plate and to the west by the Pacific Plate.
The Cocos and Nazca Plates are the remnants of the former Farallon Plate, which broke up about 23 million years ago. The boundary between the plates is marked by a hotspot under the Galapagos Islands
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