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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.
Figure 10h-2: Structure of the Earth's crust and top most layer of the upper mantle. The lithosphere consists of the oceanic crust, continental crust, and uppermost mantle. Beneath the lithosphere is the asthenosphere. This layer, which is also part of the upper mantle, extends to a depth of about 200 kilometers.