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Mohorovicic discontinuity
The boundary surface or sharp seismic-velocity discontinuity (pronounced Mo-ho-ro-vi-chich) that separates the Earth's crust from the underlying mantle. Named for Andrija Mohorovicic, the Croatian seismologist who first suggested its existence. Under Eastern Canada, it can be found at around 40 km depth.
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- Part of Speech: noun
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- Industry/Domain: Earth science
- Category: Seismology
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