Kilauea is not associated with a plate boundary, it and the other Hawaiian volcanoes are the result of a hot spot.
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.
None. Kilauea is in the middle of the Pacific Plate, It is the result of a hot spot rather than a plate boundary.
None. Kilauea and all the Hawaiian volcanoes were created by a hot spot rather than a plate boundary.
convergent plate boundary
Mount Kilauea is located at a divergent boundary, specifically at the boundary between the Pacific Plate and the North American Plate. It is part of the Hawaiian hotspot, where magma rises from the mantle to create volcanic activity. This type of boundary is characterized by tectonic plates moving apart, allowing magma to reach the surface and form shield volcanoes like Kilauea.
None. Kilauea is over a hot spot, far from the nearest plate boundary.
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.
None. Kilauea is in the middle of the Pacific Plate, It is the result of a hot spot rather than a plate boundary.
None. Kilauea and all the Hawaiian volcanoes were created by a hot spot rather than a plate boundary.
A convergent plate boundary.
convergent plate boundary
Mount Kilauea is located at a divergent boundary, specifically at the boundary between the Pacific Plate and the North American Plate. It is part of the Hawaiian hotspot, where magma rises from the mantle to create volcanic activity. This type of boundary is characterized by tectonic plates moving apart, allowing magma to reach the surface and form shield volcanoes like Kilauea.
None. Mount Tabora is not creating a boundary. It was created by a convergent plate boundary.
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The type of plate boundary creating Mount Usu is a convergent plate boundary. This supervolcano has erupted four times since 1900.
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