What is mohorovic discontinuity ?
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The Mohorovičić discontinuity, usually referred to as 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. The Moho lies almost entirely within the lithosphere.
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The Mohorovičić discontinuity, usually referred to as 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. The Moho lies almost entirely within the lithosphere.
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