No. It subducts under the continental plate.
continental volcanic arc
A convergent boundary is formed when two crustal lithospheric plates collide. This collision can result in the formation of mountain ranges, deep ocean trenches, and volcanic arcs. The type of convergent boundary that forms depends on the type of crust involved in the collision (oceanic or continental).
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.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
it would be more likely to occur at convergent ocean-continental boundary beacuse the rocks are composed with a higher silica and has much thicker continental crust.
A convergent boundary between a continental plate and an oceanic plate
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
At a convergent boundary, three types of collisions can occur: oceanic-oceanic, oceanic-continental, and continental-continental. In an oceanic-oceanic collision, one oceanic plate subducts beneath the other, forming a deep ocean trench. In an oceanic-continental collision, an oceanic plate subducts beneath a continental plate, creating volcanic arcs and mountain ranges. In a continental-continental collision, both continental plates crumple and fold, forming high mountain ranges.
Convergent boundaries , where two plates are moving toward each other, are of three types, depending on the type of crust present on either side of the boundary — oceanic or continental . The types are ocean-ocean, ocean-continent, and continent-continent.
The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.
A convergent boundary where an oceanic plate collides with a continental plate. This collision often results in the oceanic plate subducting beneath the continental plate due to its denser nature, leading to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.