It should be noted that the boundary where crust gives way to mantle is simply known as the C. Mohorovicic discontinuity.
Mohorovicic discontinuity is usually referred to as Moho. It's the boundary between the crust of the Earth and the mantle. It should be noted that it lies within the lithosphere.
Mohorovicic discontinuity is where crust gives way to mantle. It's a depth where seismic waves alter velocity and chemical composition.
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