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.
When a plate carrying oceanic crust collides with a plate carrying continental crust, the denser oceanic plate is usually subducted beneath the continental plate due to the difference in density. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity at the subduction zone.
The contiental cdrust is forced under the continental crust in a process called subduction.
When a plate carrying continental crust converges with a plate carrying oceanic crust, the denser oceanic plate is typically subducted beneath the less dense continental plate. This can lead to the formation of volcanic arcs and deep ocean trenches.
Oceanic-Oceanic.
The contiental cdrust is forced under the continental crust in a process called subduction.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
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Trench
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since the oceanic crus is thinner than the Continental crust the oceanic crust get submerged and gets destroyed while the continental crust covers the submerged part as being taken over by continental crust....//\@Rtz Z@r...