The older denser plate sinks under a deep ocean trench into the mantle. Some rock above the subducting plate melts and forms magma. Since the magma is less dense than the surrounding rock, it rises toward the surface. Eventually, the magma breaks through the ocean floor, making a volcanoe.
The water and sediments on the oceanic plate (the one being subducted) are subjected to high temperatures and pressures when they reach a certain depth. The water, combined with magma (melted sediments from both plates), works its way up through the continental plate, and volcanoes are formed where the magma breaches the surface.
As one of the plates is being subducted into the mantle, the plate melts and creates extra magma in the mantle. Because of this there is a higher pressure in the mantle and the extra magma that was melted from the plate forces it's way up to the surface. After several eruptions, volcanoes are made.
At a convergent boundry crustal plates meet, and typically one is forced under the other in a process of subduction. Crustal rock tends to melt more easily than mantle rock, it carries water and other volatiles and the friction and compression between the plates causes heating. These combine to cause the subducted plate to partially melt as it is subducted.
The melted rock is magma, which makes its way to the surface via cracks and can form explosive volcanic eruptions, as it is often viscous and has lots of volatiles.
Because of you thats why!
moderate earthquakes, volcanoes, formation of mountains and subduction zones
The Juan de Fuca plate is converging (convergent/destructive plate boundary) with the North American plate creating the Cascadia subduction zone.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Composite volcanoes most often are found near subduction zones. They can be found at either oceanic-oceanic convergent plate boundaries, oceanic-continental plate boundaries, or continental-continental plate boundaries. They are especially prevalent in the Pacific Ring of Fire. A few composite volcanoes, however, have been found at divergent boundaries and away from plate boundaries at hot spots.
Continental and Oceanic plates.
moderate earthquakes, volcanoes, formation of mountains and subduction zones
Most are found on converging
volcano occur in hot spot and diverging boundaries and converging boundaries.
Movement of lithospheric plates at convergent boundaries can result in the subduction of one plate beneath another. This subduction creates conditions for magma to form as the subducting plate melts. The rising magma then reaches the surface, leading to the formation of volcanoes.
The Juan de Fuca plate is converging (convergent/destructive plate boundary) with the North American plate creating the Cascadia subduction zone.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Composite volcanoes most often are found near subduction zones. They can be found at either oceanic-oceanic convergent plate boundaries, oceanic-continental plate boundaries, or continental-continental plate boundaries. They are especially prevalent in the Pacific Ring of Fire. A few composite volcanoes, however, have been found at divergent boundaries and away from plate boundaries at hot spots.
Continental and Oceanic plates.
Please make the question clearer. There are converging and diverging boundaries but not spreading boundaries. Plates move but don't spread. Please make the question clearer
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Subduction happens along plate boundaries which pushes up magma which then creates volcanoes.