The oceanic crust slides under the continental crust due to the differences in their densities. The continental crust is more felsic (contains more silica) which makes it lighter than the oceanic crust which is more mafic (containes more fe and mg).
Because the process of subduction is very slow, gravitational forces have a stronger effect on the more dense oceanic crust, causing this crust to be pulled under the continental crust and down into the mantle.
The oceanic crust is subducted underneath the continental crust. This process is known as subduction.
denser (Apex)
Dense oceanic crust slides under less dense continental crust
Continental crust is much thicker than oceanic crust. However, continental crust is denser and will therefore sink in subduction zones.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
denser
The oceanic crust is subducted underneath the continental crust. This process is known as subduction.
denser (Apex)
Oceanic crust sinking under a plate with continental crust
Dense oceanic crust slides under less dense continental crust
Continental crust is much thicker than oceanic crust. However, continental crust is denser and will therefore sink in subduction zones.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
density
The oceanic crust is denser than the continental crust.
oceanic and continental
This process is known as subduction and occurs at convergent plate boundaries because oceanic crust is denser than continental crust.
This is called a subduction zone.