Why is the Mohorovicic Discontinuity important?
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The Mohorovicic Discontinuity was discovered in 1909 by Andrija Mohorovicic, a Croatian seismologist. Mohorovicic realized that the velocity of a seismic wave is related to the density of the material that it is moving through. ... The higher density material below the crust became known as "Earth's mantle."
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