Mohorovičić discontinuity

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Warld cairt shawin the depth o the Moho.

The Mohorovičić discontinuity (Croatian pronunciation: [moxorôʋiːt͡ʃit͡ɕ]),[1] uisually referred tae as the Moho, is the boondary atween the Yird's crust an the mantle. Named efter the pioneerin Croatie seismologist Andrija Mohorovičić, the Moho separates baith the oceanic crust an continental crust frae unnerlyin mantle.

References[eedit | eedit soorce]

  1. Mangold, Max (2005). Aussprachewörterbuch (in German) (6th ed.). Mannheim: Dudenverlag. p. 559. ISBN 9783411040667.