The type of plate boundary creating Mount Usu is a convergent plate boundary. This supervolcano has erupted four times since 1900.
Mount Usu is created by the movement of the Pacific Plate subducting beneath the North American Plate along a convergent plate boundary. The volcanic activity at Mount Usu is a result of the melting of subducted oceanic crust and the magma rising to the surface.
USU Software was created in 1977.
USU-Brigham City was created in 1984.
De Usu Flagrorum was created in 1639.
USU Museum of Anthropology was created in 1984.
USU Eastern Prehistoric Museum was created in 1961.
USU-College of Eastern Utah was created in 1937.
convergent plates
The movement of the Pacific Plate and the North American Plate along the Aleutian Trench is causing the formation of Mount Usu. The subduction of the Pacific Plate beneath the North American Plate is resulting in volcanic activity and the formation of the volcano.
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It's a stratovolcano.
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.