it is a chemical interaction started by the water the subducted plate brings down with it which causes melting and forms magma which creates volcanoes
False. Hotspot volcanoes form above mantle plumes, which are localized upwellings of hot mantle material. Subduction zone volcanoes form due to the subduction of one tectonic plate beneath another, resulting in magma generation due to the melting of the subducted plate.
Japan formed as a result of a subduction zone.
Volcan de Fuego is related to a subduction zone. It is located along the Ring of Fire in Central America, where the Cocos Plate is subducting beneath the Caribbean Plate. This subduction process generates the magma that fuels volcanic activity at Volcan de Fuego.
Composite or stratovolcanoes typically form along subduction zones. These volcanoes are characterized by their steep-sided profile, explosive eruptions due to the presence of viscous magma, and alternating layers of lava flows and volcanic ash. Subduction zones are where one tectonic plate slides beneath another plate, leading to magma formation and volcanic activity.
Moun Cleveland formed as a result of a subduction zone, but is not a subduction zone in and of itself. A subduction zone is a feature that forms volcanoes, not a kind of volcano.
Magma is created in a subduction zone when one tectonic plate is forced beneath another plate. The intense pressure and heat cause the subducted plate to melt, forming magma that rises to the surface and can lead to volcanic activity.
About 150km from a subduction zone.
False. Hotspot volcanoes form above mantle plumes, which are localized upwellings of hot mantle material. Subduction zone volcanoes form due to the subduction of one tectonic plate beneath another, resulting in magma generation due to the melting of the subducted plate.
Volcanic arcs and oceanic trenches commonly form at subduction zones.
Japan formed as a result of a subduction zone.
Volcan de Fuego is related to a subduction zone. It is located along the Ring of Fire in Central America, where the Cocos Plate is subducting beneath the Caribbean Plate. This subduction process generates the magma that fuels volcanic activity at Volcan de Fuego.
At a convergent boundary.
Composite or stratovolcanoes typically form along subduction zones. These volcanoes are characterized by their steep-sided profile, explosive eruptions due to the presence of viscous magma, and alternating layers of lava flows and volcanic ash. Subduction zones are where one tectonic plate slides beneath another plate, leading to magma formation and volcanic activity.
Moun Cleveland formed as a result of a subduction zone, but is not a subduction zone in and of itself. A subduction zone is a feature that forms volcanoes, not a kind of volcano.
subduction zone
The opposite of a subduction zone is a divergent boundary, where tectonic plates move away from each other. This leads to the formation of new crust as magma rises from the mantle to fill the gap created by the plates moving apart.
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.