Mount Fuji, which is found in Japan is a type of island-arc volcano. It was formed by three plates, the Philippine plate, Eurasian plate and Okhotsk plate.
Mt. Fuji is a result of subduction at a convergent plate margin.
Its in Japan
1887
Its name
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Asia continet
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It was formed by the subduction of the Pacific Plate beneath the north American plate.
A subduction zone is formed.
The formation of Mount Fuji is primarily attributed to the subduction of the Pacific Plate under the Philippine Sea Plate. This tectonic activity, along with volcanic eruptions, has led to the creation of the iconic volcano over millions of years.
It is a cone volcano.