When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
subduction
Convergent plate boundaries.
When a seafloor plate collides with a continental plate, the denser seafloor plate will typically be subducted beneath the continental plate. This process can create deep ocean trenches, volcanic arcs, and earthquakes. It may also lead to the formation of mountain ranges on the continental plate.
When an oceanic plate collides with a continental plate, the denser oceanic plate usually subducts beneath the less dense continental plate due to the difference in densities. This can lead to the formation of deep oceanic trenches, volcanic arcs, and mountain ranges on the continental plate due to the intense tectonic forces generated during the collision.
the oceanic crust slides down and burns in the mantle and forms a volcano
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
The contiental cdrust is forced under the continental crust in a process called subduction.
The contiental cdrust is forced under the continental crust in a process called subduction.
subduction
a trench will form
it forms a trench
The contiental cdrust is forced under the continental crust in a process called subduction.
it subducts underneath the crustal plate
terranes are attached to the edge of a continent
himalayas
terranes are attached to the edge of a continent