The Caribbean plate has a number of convergent boundarys including subduction zone boundaries at its western margin where the Cocos plate is being forced under the North American and Caribbean plate, at it's eastern margin there is another subduction zone. Further to this there is some subduction and thrust faulting occurring at the complex southern boundary with the South American plate (where transform faulting also occurs).
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Mount Pelee is located on the Caribbean Plate boundary, specifically along the boundary between the Caribbean Plate and the North American Plate. This area is part of the Lesser Antilles subduction zone where the denser North American Plate is being subducted beneath the Caribbean Plate.
The boundary between the Caribbean and Cocos plates is a convergent boundary. The Cocos plate is being subducted beneath the Caribbean plate, resulting in volcanic activity and earthquakes along the boundary.
The North American Plate and the Caribbean Plate are on a transform boundary. This boundary is known as the North American-Caribbean Plate boundary, where the plates slide past each other horizontally. This motion results in frequent earthquakes in the region.
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.
convergant
the mid ocean ridges cause the magma to form at a convergent plate boundary.
Mount Pelee is located on the Caribbean Plate boundary, specifically along the boundary between the Caribbean Plate and the North American Plate. This area is part of the Lesser Antilles subduction zone where the denser North American Plate is being subducted beneath the Caribbean Plate.
The boundary between the Caribbean and Cocos plates is a convergent boundary. The Cocos plate is being subducted beneath the Caribbean plate, resulting in volcanic activity and earthquakes along the boundary.
The North American Plate and the Caribbean Plate are on a transform boundary. This boundary is known as the North American-Caribbean Plate boundary, where the plates slide past each other horizontally. This motion results in frequent earthquakes in the region.
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.
coliding boundary
The type of plate boundary the Vesuvius is located on it a subduction zone in latitude 40.9n and 14e. It lies on the convergant boundry of the African and Euasian plates.
Yes, It is on the Caribbean Plate
It is a subduction zone.
The Atlantic Plate is being subducted beneath the eastern Caribbean Plate.