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The Mohorovicic Discontinuity, commonly called the “Moho,” is recognized as the boundary zone between Earth's crust and the mantle. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate. https://loom.ly/qDTmxag | EarthScope Consortium
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The Mohorovicic Discontinuity, commonly called the “Moho,” is recognized as the boundary zone between Earth's crust and the mantle. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate. https://loom.ly/qDTmxag | EarthScope Consortium
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