Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Most are found on converging
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Volcanoes that form on converging plate boundaries are typically stratovolcanoes or composite volcanoes. These volcanoes are formed by the subduction of one tectonic plate beneath another, leading to the formation of a volcanic arc and explosive eruptions due to the melting of the subducted plate. Examples include the Cascade Range in the U.S. and the Andes in South America.
the plate of your mom
Volcanoes form on tectonic plates at plate boundaries where magma from the Earth's mantle can rise to the surface. This typically occurs at divergent or convergent plate boundaries where there is movement and interaction between the plates, leading to volcanic activity.
Several things are characteristic of plate boundaries. Mountain and volcanoes are common at converging plate boundaries, as well as faults and earthquakes. mid oceanic ridges form when the edges of oceanic tectonic plates spread appart from each other. Island arcs form near the edges of a subducting tectonic plate.
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dining table plates
volcanos mostly form on tectonic plate boundaries and hot stops
Volcanoes primarily form at tectonic plate boundaries, particularly at divergent and convergent boundaries. At divergent boundaries, tectonic plates move apart, allowing magma to rise and create new crust, often seen in mid-ocean ridges. At convergent boundaries, one plate subducts beneath another, leading to melting and volcanic activity. Therefore, while volcanoes can form at various plate boundaries, they do not always form on a single type of plate.
Hot spots!
The Convergent boundary forms a subduction zone. When the heavier plate reaches 100km the water is released from the submerged plate, and the mantle starts to melt. The mantle rises and a volcano forms on the lighter side plate. Unless it is a continent-continent convergent plate where mostly mountains are forms.