Mount Irazú has several craters, with the main ones being the Diego de la Haya crater and the Playa Hermosa crater. Overall, the volcano has at least 10 major craters, each varying in size and activity levels.
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.
No. Mount Tambora is in the shape of a caldera form from a stratovolcano.
it is a cone
Mount Hood is a stratovolcano, which typically has a symmetrical conical shape with a steep summit and gradual slopes.
Mount Irazú has several craters, with the main ones being the Diego de la Haya crater and the Playa Hermosa crater. Overall, the volcano has at least 10 major craters, each varying in size and activity levels.
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.
to old
11,260 feet
YES!
A cone shape.
No. Mount Tambora is in the shape of a caldera form from a stratovolcano.
it is a cone
Mount Hood is a stratovolcano, which typically has a symmetrical conical shape with a steep summit and gradual slopes.
Roughly 11260 feet or 3432 meters.
Mount Aneto is a mountain, so it does not have a standard geometric shape. It is part of the Pyrenees mountain range and has a rugged, natural shape with peaks and valleys.
No.