What Is Mohorovicic 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. Named after the pioneering Croatian seismologist Andrija Mohorovičić, the Moho separates both the oceanic crust and continental crust from underlying mantle.
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The boundary surface between the earth's crust and the mental, lying at a depth of about 10-12km under the ocean bed and 40-50km under the continents.
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