Moho | Energy Glossary

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Moho

1. n. []

The boundary between the crust and the mantle of the Earth, which varies from approximately 5 km [3 miles] under the midoceanic ridges to 75 km [46 miles] deep under the continents. This boundary, commonly called "the Moho," was recognized in 1909 by Croatian seismologist Andrija Mohorovicic on the basis of its abruptly higher compressional wave (P-wave) velocity.

Alternate Form: Mohorovicic discontinuity

Diagram of layers of the Earth.