The Mohorovičić discontinuity, often referred to as the Moho discontinuity, is the boundary between the Earth's crust and the underlying mantle. It represents a significant change in seismic wave velocities, marking the transition from the less dense crust to the denser mantle beneath. Named after the Croatian seismologist Andrija Mohorovičić who first identified it in 1909, the Moho discontinuity is crucial in understanding the Earth's internal structure.
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Explanation:
The Mohorovičić discontinuity, often referred to as the Moho discontinuity, is the boundary between the Earth's crust and the underlying mantle. It represents a significant change in seismic wave velocities, marking the transition from the less dense crust to the denser mantle beneath. Named after the Croatian seismologist Andrija Mohorovičić who first identified it in 1909, the Moho discontinuity is crucial in understanding the Earth's internal structure.