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Mt. Hood is an example of a convergent boundary, where the North American Plate is colliding with the Juan de Fuca Plate, leading to the formation of the Cascade Mountain Range.
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.
Mount Merapi is a convergent boundary type, specifically a subduction zone where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction has led to the explosive volcanic activity and frequent eruptions characteristic of Mount Merapi.
Mount Veniaminof in Alaska is located along the Aleutian subduction zone, which is a convergent plate boundary where the Pacific Plate is being subducted beneath the North American Plate. This subduction zone is characterized by frequent volcanic activity and seismic events due to the collision of the two tectonic plates.
Mount Pavlof in Alaska is located along the boundary between the Pacific Plate and the North American Plate. The subduction of the Pacific Plate beneath the North American Plate in this region leads to volcanic activity, resulting in the formation of Mount Pavlof.
Mount Hood is not located at a convergent boundary. Instead, it is part of the Cascade Range, which is formed by volcanic activity associated with the subduction of the Juan de Fuca Plate beneath the North American Plate. This tectonic setting creates a series of stratovolcanoes, including Mount Hood, but the specific boundary itself is classified as a convergent boundary due to the subduction process. Therefore, while Mount Hood is linked to a convergent boundary, it is not a boundary itself.
Mount Hood is formed by a convergent boundary where the Juan de Fuca tectonic plate is being subducted beneath the North American plate. This subduction causes magma to rise and create the volcanic activity that forms Mount Hood.
Mount Merapi is near a convergent plate boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate.
No, Mount Cameroon is not on a divergent plate boundary. It is located on the African Plate near the boundary with the smaller Oku Plate to the northwest.
mount etna is on asubduction plate boundary under the african and eurasian plate
Mount Pinatubo is on a destructive plate boundary; it is above a subduction zone
African plate
Mt. Hood is an example of a convergent boundary, where the North American Plate is colliding with the Juan de Fuca Plate, leading to the formation of the Cascade Mountain Range.
eruasion plate
Mount Wrangell is situated on a convergent plate boundary, specifically where the Pacific Plate is subducting beneath the North American Plate. This boundary is associated with the formation of the Aleutian Islands and the Alaska Range of mountains.
None. Mount Tabora is not creating a boundary. It was created by a convergent plate boundary.
Mount Erebus is located on the boundary of the Antarctic Plate and the Pacific Plate. The movement of these plates against each other creates a convergent boundary, where the Pacific Plate is being forced beneath the Antarctic Plate. This process, known as subduction, is responsible for the volcanic activity at Mount Erebus.