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This is the Continental crust (also some Oceanic), as the crust part of the Lithosphere.
It is broken into tectonic plates. Two types are the Continental Crust and the Oceanic Crust.
oceanic crust.
A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.
Lithosphere is categorized into two sections. They are crust and upper most mantle. Crust includes continental and oceanic crust and technology.
They can be either continental or oceanic crust.
This is the Continental crust (also some Oceanic), as the crust part of the Lithosphere.
It is broken into tectonic plates. Two types are the Continental Crust and the Oceanic Crust.
The oceanic crust is subducted underneath the continental crust. This process is known as subduction.
oceanic crust.
A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
Lithosphere is categorized into two sections. They are crust and upper most mantle. Crust includes continental and oceanic crust and technology.
northeast
Oceanic crust sinking under a plate with continental crust
the oceanic crust is 0.