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Mount Usu in Japan typically erupts with andesitic lava, which is a type of intermediate lava with a higher silica content compared to basaltic lava. Andesitic lava flows tend to be slower-moving and more viscous than basaltic lava.
Mt. Usu is a stratovolcano located in Hokkaido, Japan. It was formed through a series of volcanic eruptions over time, with its most recent eruption occurring in 2000.
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Mount St Helens is a composite cone (strato) volcano.
Mt. Usu is formed by the subduction of the Pacific Plate beneath the Eurasian Plate. This subduction process creates magma which rises to the surface, forming volcanoes like Mt. Usu. The volcanic activity in the region is a result of this tectonic plate movement.
It's a stratovolcano.
a cinder cone
Mt. Pelee is a Cinder Cone Volcano.
Mount Usu in Japan typically erupts with andesitic lava, which is a type of intermediate lava with a higher silica content compared to basaltic lava. Andesitic lava flows tend to be slower-moving and more viscous than basaltic lava.
cinder cone
Stratovolcano
1300
Mt. Usu is a stratovolcano located in Hokkaido, Japan. It was formed through a series of volcanic eruptions over time, with its most recent eruption occurring in 2000.
Mount Trident is a cinder cone type of volcano.
It's a caldera... check wikipedia///
where will i get this stupid answer? really you guys useless idiots
It is a stratovolcano, akin to Mt. Rainier in Washington State.