Mohorovičić discontinuity

E1418029 UNEXPLORED

The Mohorovičić discontinuity is the boundary within the Earth where seismic wave velocities abruptly increase, marking the transition between the crust and the mantle.

All labels observed (2)

Label Occurrences
Moho discontinuity 1
Mohorovičić discontinuity canonical 1

How this entity was disambiguated

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Earth's crust innerBoundary Mohorovičić discontinuity
Airy isostasy model involves Moho discontinuity
linked to: Mohorovičić discontinuity