Answer:
The seismic-velocity discontinuity between the Earth's mantle and core. The boundary is at a depth of about 2 600 km and is thought to have surface irregularities of a few kilometres. From: Gutenberg discontinuity in A Dictionary of Earth Sciences »
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Answer:
Core–mantle boundary
The seismic-velocity discontinuity between the Earth's mantle and core. The boundary is at a depth of about 2 600 km and is thought to have surface irregularities of a few kilometres. From: Gutenberg discontinuity in A Dictionary of Earth Sciences »