When there is oceanic-oceanic convergence, one layer of oceanic lithosphere is subducted. This not only introduces water, which lowers the melting temperature of the asthenosphere, but can create an island with a volcano. This occurs when the hot magma rises from the subduction zone and build up in size. This would not have any specific name. If the volcano was situated on a hot spot, however, it would form linear island chains.
I think its a chain of volcanoes form when oceanic crust subducts beneath other oceanic crust on an adjacent plate. Hope this helps (:
both volcanoes are located near the African plate boundary
The two plate boundaries are the Juan de Fuca plate and the North American Plate.
My best answer that my college teacher taught me is in the oceanic plate.HOPE THIS HELPED! : D
Galeras Volcano is formed along Nazca and South American plates. It is a convergent boundary and is oceanic-continental. If you need more info. Go to geology.com
The Transform plate boundary commonly forms a chain of volcanoes - Professer Humifiken
Convergent with the oceanic plate subducting under the continental plate.
Oceanic-to-Oceanic plate boundary triggers the formation of active volcanoes as magma rises beneath the surface.Transform plate boundaries trigger the formation of active volcanoes as magma rises beneath the surface.
In an oceanic-continental convergent plate boundary, an oceanic plate is subducted beneath a continental plate due to differences in density. This process can lead to the formation of deep ocean trenches, volcanic arcs on the continental plate, and earthquakes. The subduction of the oceanic plate can also cause melting of rock, leading to the formation of magma that can erupt as volcanoes on the continental plate.
Volcanoes on continents can develop at path convergent and divergent boundaries. They can occur where an oceanic plate subducts under a continental plate, producing a volcanic arc such as in the Cascade Range. Volcanoes can also occur in areas of rifting, such as Africa's Great Rift Valley, a developing divergent boundary. Where two oceanic plates converge volcanoes can develop underwater and eventually form volcanic islands. Volcanoes can also develop away from a plate boundary over a hot spot.
A string of volcanoes along an ocean-to-ocean convergent boundary is called a volcanic island arc. This forms when one oceanic plate subducts beneath another oceanic plate, leading to volcanic activity along the subduction zone. Examples include the Aleutian Islands in Alaska and the Japanese archipelago.
A convergent boundary forms when an oceanic plate is pushed under a continental plate. This process, known as subduction, can result in the formation of deep ocean trenches, volcanic arcs, and earthquakes.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
convergent oceanic oceanic
When an oceanic plate converges with a continental plate, the oceanic plate slips under the continental one and into the mantle in a process called subduction. The area will be prone to large earthquakes and tsunamis. A chain of volcanoes will form on the continent.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
volcanoes are caused by subduction. it could be an oceanic plate sub-ducting under a continental plate which would result in a coastal volcano or it could be an oceanic plate sub-ducting under another oceanic plate, which would result in a volcanic island.