At the subduction zones.
Due to the ancient boundaries entering the lithosphere thus being recycled back through magma pockets.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
What part in the egg is the lithosphere
you make the lithosphere with the mantle and the asthenophere.
New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones.
no
Due to the ancient boundaries entering the lithosphere thus being recycled back through magma pockets.
the lithosphere is the solid upper part of the mantle and the crust, which are spilt up into plates on the earth surface, which are constantly moving. at destructive plate boundaries the plates can get subducted and "recycled" into the mantle, hence lithosphere is destroyed. at mid ocean ridges new crust (lithopshere) is constantly being made. this all leads to the dynamic and continuous cycles of lithosphere being destroyed and created, hence continually changing.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The uppermost mantle and the crust makes the lithosphere.
The difference between the core and the lithosphere is the core is on the top of the lithosphere and the lithosphere is on the bottom of the core
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
lithosphere.
division of lithosphere
Lithosphere (apex)
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.