Question

What is the Mohorovicic discontinuity and where is it found?

Answer 1

The Mohorovicic Discontinuity or "Moho" is the boundary between the cryst and the mantle. It lies on average 30-50 km below the surface on cobtinents, but 5-10 km under the oceans.

Explanation:

A map of the depth of the crust down to the Moho is available at https://en.wikipedia.org/wiki/Mohorovičić_discontinuity.