Concept
Mohorovicic Discontinuity
MOH-hoh (short form); moh-hoh-ROH-vih-chich (full)
Also Known As The Moho
Seismology
The boundary separating the Earth's crust from its mantle, discovered by Andrija Mohorovicic from the way seismic waves from a 1909 earthquake reflected and refracted as they crossed it. Its depth varies from about 5 kilometers under the ocean floor to several tens of kilometers under mountain ranges. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
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In Discipline
Source Andrija Mohorovicic (Wikipedia)
Proposed By
Source Andrija Mohorovicic (Wikipedia)
Sources
1. Andrija Mohorovicic (Wikipedia)
Wikimedia FoundationBiography sectionQuote, Biography section
He was the first to establish, based on the evidence from seismic waves, the discontinuity that separates the Earth's crust from its mantle.
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