ls it formed due to a hot spot or a plate boundary Komagatake
Kilauea is a result of a hot spot, not subduction. It is located on the Big Island of Hawaii, which sits over a volcanic hot spot in the Earth's mantle. This hot spot produces magma that rises to the surface, causing the formation of volcanoes like Kilauea. In contrast, subduction involves one tectonic plate sliding beneath another, leading to different volcanic activity.
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
No. The volcanic activity in Japan is associated with a subduction zone.
A volcanic hot spot forms from upwelling magma usually due to the subduction of a tectonic plate. As plates move over this area new volcanoes are formed. +++ A hot spot alone is the top of a convection plume in the Mantle, not above subduction. This type of hot spot can lead to continental rifting.
Oshima volcano, like many in Japan, is primarily the result of subduction rather than a hot spot. This is due to the convergence of the Philippine Sea Plate and the Eurasian Plate, leading to volcanic activity as the subducting plate melts and generates magma. While there are hot spot volcanic activities elsewhere, the context of Oshima's formation is largely linked to the tectonic processes associated with subduction.
ls it formed due to a hot spot or a plate boundary Komagatake
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
No. The volcanic activity in Japan is associated with a subduction zone.
No. Mount Unzen, like the other volcanoes in Japan, was formed by a subduction zone.
A volcanic hot spot forms from upwelling magma usually due to the subduction of a tectonic plate. As plates move over this area new volcanoes are formed. +++ A hot spot alone is the top of a convection plume in the Mantle, not above subduction. This type of hot spot can lead to continental rifting.
Close to a tectonic plate subduction zone, a tectonic spreading zone or a localised 'hot spot'.
hot spot
Krakatoa is not associated with a hot spot. It is associated with a subduction zone.
No. Hot spots and subduction zones are two separate geogolgic settings in which volcanoes can form. Some hot spots may develop as a result of activity in a subduction zone, and continue activity after subduction has ended or move away.
Mount Fuji is not associated with a hot spot. It is associated with a subduction zone.
Composite volcanoes, also known as stratovolcanoes, are most likely to form in subduction zones where one tectonic plate is being forced beneath another. This is because the subduction zone creates a favorable environment for the magma to rise and accumulate. Examples of composite volcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.