what is mohorovicic discontinuity
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The Mohorovičić discontinuity, moh-hoh-ROH-veech-itch, usually referred to as the Moho discontinuity or the Moho, is the boundary between the Earth's crust and the mantle. It is defined by the distinct change in velocity of seismological waves as they pass through changing densities of rock.
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the boundary surface between the earth's crust and the mantle, lying at a depth of about 10–12 km under the ocean bed and 40–50 km under the continents.
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