it was a convergent of divergent because it is a stratovolcano
convergent plate boundary
Galeras Volcano is formed along Nazca and South American plates. It is a convergent boundary and is oceanic-continental. If you need more info. Go to geology.com
Mount Fuji is a composite volcano.
A composite volcano or Strata Volcano.
No. A volcano is not a plate boundary. Most volcanoes on land are associated with convergent boundaries, but many are associated with divergent boundaries and others with hot spots.
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Composite cone
it was a convergent of divergent because it is a stratovolcano
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.
Volcanoes can form at convergent boundaries, divergent boundaries, and at hot spots away from any plate boundary.
The Villarrica Volcano is located on a convergent boundary where the South American tectonic plate is subducting beneath the Nazca plate. This subduction leads to the formation of the Andes mountain range and associated volcanic activity.
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.
Volcanoes are typically associated with divergent plate boundaries, where plates are moving apart from each other. This movement allows magma to rise to the surface and creates volcanic activity.
Normally a Divergent boundary because as the plates diverge, lava spews out, but they can also form at a Convergent boundary, or, although less likely, a transform boundary.
Popocatepetl is situated along a convergent plate boundary where the Cocos Plate is subducting beneath the North American Plate.
A stratovolcano, also known as a composite volcano, is the type of volcano that occurs along a convergent plate boundary. These volcanoes are typically steep-sided and have explosive eruptions due to the presence of viscous magma.