The Moho discontinuity is the boundary between the Earth's crust and the mantle. It has been named so because it was discovered by a Croatian scientist, Andreaja Mohorovicic. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate.
The Mohorovičić discontinuity, often referred to as the Moho discontinuity, is the boundary between the Earth's crust and the underlying mantle. It was named after Andrija Mohorovičić, a Croatian seismologist who first identified this seismic boundary. The Moho is characterized by an abrupt increase in seismic wave velocity, indicating a change in composition from the lighter, rigid crust to the denser, more fluid-like mantle beneath.
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Answer:
The Moho discontinuity is the boundary between the Earth's crust and the mantle. It has been named so because it was discovered by a Croatian scientist, Andreaja Mohorovicic. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate.
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Answer:
The Mohorovičić discontinuity, often referred to as the Moho discontinuity, is the boundary between the Earth's crust and the underlying mantle. It was named after Andrija Mohorovičić, a Croatian seismologist who first identified this seismic boundary. The Moho is characterized by an abrupt increase in seismic wave velocity, indicating a change in composition from the lighter, rigid crust to the denser, more fluid-like mantle beneath.
Okay I will wait, till we will be talking like this in brainly!