Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
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.
It forms a convergent boundary with the South American Plate, divergent.
No, the Santa Maria volcano is not located at a divergent plate boundary; it is situated in a convergent plate boundary region where the Cocos Plate is being subducted beneath the North American Plate. This subduction process is responsible for the formation of the volcanic activity in the region. Santa Maria is a stratovolcano, and its eruptions are primarily due to the melting of the subducted oceanic crust.
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.
Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
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.
Convergent, divergent, or maybe a transform boundary. Choose any one you want to.
It forms a convergent boundary with the South American Plate, divergent.
Costa Rica is a convergent plate boundary, specifically a subduction zone where the Cocos Plate is being subducted beneath the Caribbean Plate. This geologic process is responsible for the country's high levels of seismic and volcanic activity.
It forms a convergent boundary with the South American Plate, divergent.
Popocatepetl is located on the western edge of the North American Plate, near the triple junction where the Cocos Plate, North American Plate, and Pacific Plate meet. This makes it a convergent boundary where the Cocos Plate is subducting beneath the North American Plate. The subduction of the Cocos Plate beneath the North American Plate is responsible for the volcanic activity at Popocatepetl.
It forms a convergent boundary with the South American Plate, divergent.
No, the Santa Maria volcano is not located at a divergent plate boundary; it is situated in a convergent plate boundary region where the Cocos Plate is being subducted beneath the North American Plate. This subduction process is responsible for the formation of the volcanic activity in the region. Santa Maria is a stratovolcano, and its eruptions are primarily due to the melting of the subducted oceanic crust.
The Andes are a result of the convergent boundary between the Nazca and South American 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.
Convergent on the western perimeter, divergent on the Easter perimeter.