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The upper mantle is made of peridotite and eclogite rock and extends from the Moho to a depth of 400km. The earth's crust and uppermost mantle together form the lithosphere. The lithosphere makes up the plates of plate tectonic theory. The lithosphere averages about 70 kilometers thick beneath continents.
The gases evolved during the melting of Earth's mantle have a large effect on the composition and size of Earth's atmosphere. Uppermost mantle. A thin crust, the lower part of the lithosphere, surrounds the mantle and is about 5 to 75 km thick. There are two main zones in the upper mantle. The uppermost mantle plus overlying crust are relatively rigid and form the lithosphere, an irregular layer with a maximum thickness of perhaps 200 km, of which the uppermost mantle is 120 to 50 km thick.