What is Mohorovicic discontinuity.
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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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The Mohorovicic discontinuity is the boundary between the crust and the mantle; it normally lies entirely within the lithosphere, but at the mid-Atlantic Ridge, it defines the boundary between the lithosphere and athenosphere. The Moho lies typically 5 km below the ocean floor, and 30–50 km beneath continents.
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