No, but the last time it erupted was in 1936.
The Falcon Volcano on the Tonga Islands are in the Indo-Australian Plate- a convergent boundary.
No, Irazu is not a divergent boundary. Irazu is a volcano located in Costa Rica, and it is associated with the subduction boundary where the Cocos Plate is being pushed below the Caribbean Plate.
A diverging is the type of plate boundary that the Hekla volcano formed. Hekla last erupted in 2000. It is located in Iceland. ADDED. Also called a "constructive" plate boundary, because the upwelling magma adds rock to the edges of the two plates.
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.
The Taal Volcano is located on a divergent plate boundary, specifically the boundary between the Eurasian Plate and the Philippine Sea Plate. This boundary is where the two plates are moving away from each other, creating volcanic activity due to the upwelling of magma from the mantle.
rezy
it is on a divergent boundary
It isnt a volcano
A volcano.
The Falcon Volcano on the Tonga Islands are in the Indo-Australian Plate- a convergent boundary.
The Falcon Volcano on the Tonga Islands are in the Indo-Australian Plate- a convergent boundary.
convergent
Eyjafjallajokull volcano is located on the divergent boundary between the North American Plate and the Eurasian Plate in Iceland.
No, Irazu is not a divergent boundary. Irazu is a volcano located in Costa Rica, and it is associated with the subduction boundary where the Cocos Plate is being pushed below the Caribbean Plate.
A diverging is the type of plate boundary that the Hekla volcano formed. Hekla last erupted in 2000. It is located in Iceland. ADDED. Also called a "constructive" plate boundary, because the upwelling magma adds rock to the edges of the two plates.
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.
The Taal Volcano is located on a divergent plate boundary, specifically the boundary between the Eurasian Plate and the Philippine Sea Plate. This boundary is where the two plates are moving away from each other, creating volcanic activity due to the upwelling of magma from the mantle.