Continental margin
Continental Slope
continental slope
The oceanic crust is denser than the continental crust.
It is created at mid-oceanic ridges (divergent boundaries) and it is destroyed at subduction zones (convergent boundary between oceanic crust and continental crust).
The oceanic crust is subducted underneath the continental crust. This process is known as subduction.
oceanic crust
Continental Slope
continental slope
continental slope
continental slope
Oceanic to oceanic- one plate sinks under the other Oceanic- Continental ocean crust sinks under the other
Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.
The oceanic crust is denser than the continental crust.
At a convergent boundary between oceanic and continental crust where subduction is occurring.
It is created at mid-oceanic ridges (divergent boundaries) and it is destroyed at subduction zones (convergent boundary between oceanic crust and continental crust).
The oceanic crust is subducted underneath the continental crust. This process is known as subduction.
tides will occur.