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Subduction of Indi-Australian plate under the Eurasian plate cause Mount Sinabung

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What type of boundary is mount sinabung on top of?

Mount Sinabung is located on the boundary between the Indo-Australian Plate and the Eurasian Plate. This region is characterized by subduction, where the Indo-Australian Plate is being forced beneath the Eurasian Plate, leading to volcanic activity. Sinabung is classified as a stratovolcano, typical of subduction zones, where magma accumulates due to the melting of the subducted plate.


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Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.


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What type of plate boundary does mt Kilimanjaro sit on?

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What plates are causing mount sinabung?

Mount Sinabung, located in Indonesia, is primarily influenced by the interaction of the Indo-Australian Plate and the Eurasian Plate. The subduction of the Indo-Australian Plate beneath the Eurasian Plate creates the volcanic activity associated with Sinabung. This tectonic setting leads to the formation of magma and the eruption of the volcano. Overall, it is the complex dynamics of these tectonic plates that drive the volcanic activity at Mount Sinabung.


What type of plate is creating mt fuji?

Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.