In convergences between two oceanic plates OR between an oceanic and a continental plate, the more dense plate subducts under the less dense plate and moves toward the mantle. As the geothermal gradient increases with depth, the subducting plate is exposed to higher and higher temperatures. The oceanic crust undergoes partial melting from exposure to these increased temperatures, and due to the presence of water in the subducting plate. Lithostatic pressure,and the low density of the magma cause it to rise toward the surface. Some magma may solidify underground before reaching the surface; some magma, however, finds its way to the surface, and produces a volcano.
Plates do not cause volcanoes. Volcanoes generally form at the boundaries between plates. They form at convergent and divergent boundaries.
Convergent boundaries form mountains and volcanoes.
Underwater volcanoes and mountains can form at both convergent and divergent boundaries.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
The convergent mountains usually come in ranges, rather than solitary peaks.
Plates do not cause volcanoes. Volcanoes generally form at the boundaries between plates. They form at convergent and divergent boundaries.
Convergent boundaries form mountains and volcanoes.
Underwater volcanoes and mountains can form at both convergent and divergent boundaries.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
No. Volcanoes do not form at transform boundaries. Volcanic islands can form at convergent boundaries and at hot spots.
hot spots and convergent boundaries
The convergent mountains usually come in ranges, rather than solitary peaks.
at the edge of plate collisions
they both form volcanoes and earthquakes
Composite cone volcanos are the most common.. Shielding and other types are results from a divergent boundary.
It collides with the upper mantle that forms volcanoes with violent eruptions
pacific