Convergent
Mt Fuji is located on three plates. Those three plates are: Amurian, Okhotsk, and the Filipino located directly below Fuji.
The boundary of Mount Fuji is created by the subduction of the Pacific Plate underneath the North American Plate. This subduction has led to the formation of the volcanic arc that includes Mount Fuji.
Mount Fuji is located on the convergent boundary between the Pacific Plate and the Philippine Sea Plate. This boundary is a subduction zone, with the Philippine Sea Plate being forced beneath the Pacific Plate. The intense geologic activity in this region is responsible for the formation of Mount Fuji and the volcanic activity in the area.
Mount Fuji is not created at a destructive boundary. It is actually a stratovolcano located at a convergent boundary where the Pacific Plate subducts beneath the Eurasian Plate. The subduction of the oceanic plate beneath the continental plate creates conditions for magma to rise and form the volcano. Destructive boundaries typically involve the collision or subduction of tectonic plates, leading to volcanic activity.
Mount Fuji is located on a convergent boundary between the Eurasian Plate and the Philippine Sea Plate. This boundary is a type of subduction zone, where one tectonic plate is being forced beneath another.
Mt Fuji is located on three plates. Those three plates are: Amurian, Okhotsk, and the Filipino located directly below Fuji.
mount Fuji lies on the Eurasian plate.
eurasian plate
Japan.
Mount Fuji in Japan formed in several stages due to subduction at the convergence of three plates: the Pacific plate, Philippine plate and Eurasian plate. The last eruption was in 1707-1708, but any new eruption from the summit crater could add to the height of the volcano.
they are meltig down and new ones are forming
your, nan
The boundary of Mount Fuji is created by the subduction of the Pacific Plate underneath the North American Plate. This subduction has led to the formation of the volcanic arc that includes Mount Fuji.
Mount Fuji is located on the convergent boundary between the Pacific Plate and the Philippine Sea Plate. This boundary is a subduction zone, with the Philippine Sea Plate being forced beneath the Pacific Plate. The intense geologic activity in this region is responsible for the formation of Mount Fuji and the volcanic activity in the area.
Mt. Fuji is a result of subduction at a convergent plate margin.
it is the pacific plate and the urasion plate
Mount Fuji is not created at a destructive boundary. It is actually a stratovolcano located at a convergent boundary where the Pacific Plate subducts beneath the Eurasian Plate. The subduction of the oceanic plate beneath the continental plate creates conditions for magma to rise and form the volcano. Destructive boundaries typically involve the collision or subduction of tectonic plates, leading to volcanic activity.