The oceanic plate goes under the continental plate and into the mantle in a process known as subduction. This results in the formation of mountains and volcanoes on the continental plate.
When a continental and oceanic plate collide, the denser oceanic plate is typically forced underneath the less dense continental plate in a process known as subduction. This can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity. The collision can also result in the uplift of mountains along the continental plate's edge.
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When a oceanic plate collides with a continental plate, the denser oceanic plate is usually subducted beneath the lighter continental plate. This can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches. The collision can also lead to earthquakes and the release of magma.
Oceanic-continental plate boundary: where an oceanic plate and a continental plate collide, causing the oceanic plate to subduct beneath the continental plate. Oceanic-oceanic plate boundary: occurs when two oceanic plates collide, with one plate usually subducting beneath the other. Continental-continental plate boundary: where two continental plates collide, leading to the formation of mountain ranges through intense compression and uplifting of the crust.
When dense oceanic plates collide with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of deep ocean trenches, volcanic arcs, and mountain ranges on the continental plate. Subduction zones are also associated with earthquakes and volcanic activity.
This phenomenon, known as subduction, occurs because oceanic plates are denser and thinner than continental plates. When the two plates collide, the denser oceanic plate is forced beneath the less dense continental plate due to gravitational pull. This process results in the oceanic plate descending into the mantle, leading to the formation of deep ocean trenches and volcanic arcs.
Its when the oceanic crust and the continental crsut colide together.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
Yes, it "dives" under the continental crust and back into the mantle.
Subduction occurs when one tectonic plate moves underneath another plate at a convergent boundary. This typically happens at deep ocean trenches where the denser oceanic plate is forced beneath the less dense continental plate. Subduction is a key process in the cycle of plate tectonics, leading to the formation of volcanic arcs and earthquakes.