The density of Earth's lithosphere is 2.5 gm/cm^3
the density of the lithosphere is 3.6g/cm^3
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.
The asthenosphere is a flowing solid. It's sort of a liquid and a solid.
Do you mean spreading centres or oceanic ridges, where the oceanic lithosphere is renewed by hot, less dense rock rising in convection zones.
The Lithosphere is the ridged layer of Earth that is about 100 km think and generally less dense than the material below it. This layer is the tectonic plates the move along on the anthesphere.
lithosphere, hydrosphere, atmosphere (most dense to least dense)
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 asthenosphere is more dense than the lithosphere.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
Lithosphere
The lithosphere is cold and brittle whereas the asthenosphere is hot and dense.
The Lithosphere Floats on top of the asthenosphere because it is less dense.
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.
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.
It is found in the earth
The asthenosphere.
Continental lithosphere is thicker and less dense than oceanic lithosphere. Continental crust is primarily composed of granitic rock while oceanic crust is composed primarily of basaltic rock.