The Moho discontinuity is the boundary between the Earth's crust and the mantle. It has been named so because it was discovered by a Croatian scientist, Andreaja Mohorovicic. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate.
Mohorovicic Discontinuity: This is the transition zone between the crust and the mantle. Repetti Discontinuity: This separates the upper mantle from the lower mantle. Gutenberg Discontinuity: This is the transition zone between the lower mantle and the outer core.
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Answer:
The Moho discontinuity is the boundary between the Earth's crust and the mantle. It has been named so because it was discovered by a Croatian scientist, Andreaja Mohorovicic. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate.
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Explanation:
Mohorovicic Discontinuity: This is the transition zone between the crust and the mantle. Repetti Discontinuity: This separates the upper mantle from the lower mantle. Gutenberg Discontinuity: This is the transition zone between the lower mantle and the outer core.
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