The pacific plate and the cocos plate
The Juan de Fuca Plate and the Cocos Plate originally belonged to the Farallon Plate. The Farallon Plate was a large oceanic plate that existed between the Pacific Plate and the North American Plate. Over time, much of the Farallon Plate was subducted beneath the North American Plate, leading to the formation of the Juan de Fuca and Cocos Plates as remnants of this once larger plate.
Cerro Negro is located on the boundary between the Caribbean Plate and the Cocos Plate in Nicaragua. This boundary is characterized by the subduction of the Cocos Plate beneath the Caribbean Plate, leading to volcanic activity in the region.
No, Arenal is not located on a divergent boundary. It is a volcano in Costa Rica situated on the tectonic boundary between the Caribbean Plate and the Cocos Plate, which is a convergent boundary where the Cocos Plate is subducting beneath the Caribbean Plate.
The Cocos Plate is mainly located beneath the Pacific Ocean and is associated with the countries of Mexico, Guatemala, Costa Rica, Nicaragua, and Panama in Central America.
Cocos Plate is moving towards the north-east.
Cocos Plate is moving towards the north-east.
The Cocos Plate.
cocos plate
The Pacific and Cocos plate.
They don't move in a specific direction. Every plate moves in it's own direction and sometimes they can change directions.
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the cocos plates are located next to the caribbean plate
Cocos plate and the African plate
The pacific plate and the cocos plate
The Pacific and Cocos plate.
Cerro Negro is located on the boundary between the Caribbean Plate and the Cocos Plate in Nicaragua. This boundary is characterized by the subduction of the Cocos Plate beneath the Caribbean Plate, leading to volcanic activity in the region.