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.
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Mt Fuji is located on three plates. Those three plates are: Amurian, Okhotsk, and the Filipino located directly below Fuji.
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Beauty is subjective and both Mount Mayon and Mount Fuji are stunning in their own unique ways. Mount Mayon's perfect cone shape and lush surroundings make it visually captivating, while Mount Fuji's symmetrical form and cultural significance in Japan add to its allure. Ultimately, the beauty of each mountain is in the eye of the beholder.
The Pacific Plate is causing Mount Erebus to form. This plate is moving over a stationary hotspot beneath the Earth's crust, creating a chain of volcanoes including Mount Erebus in Antarctica.
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The tectonic plates of course
The Pacific Plate is subducting beneath the Eurasian Plate, which is causing the formation of Mount Fuji. This subduction process leads to magma rising to the surface and eventually forming the volcanic mountain.
Mount hoot is formed by the Juan de Fuca Plate subducting under the North American Plate.
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.