Explain the Moho discontinuity on the basis of seismic evedenace

1.	Explain the Moho discontinuity on the basis of seismic evedenace
Answer» Answer: This seismic DISCONTINUITY is now know as the Moho (much EASIER than "Mohorovicic seismic discontinuity") It is the BOUNDARY between the felsic/mafic crust with seismic velocity around 6 km/sec and the denser ultramafic mantle with seismic velocity around 8 km/sec.

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Answer:

This seismic DISCONTINUITY is now know as the Moho (much EASIER than "Mohorovicic seismic discontinuity") It is the BOUNDARY between the felsic/mafic crust with seismic velocity around 6 km/sec and the denser ultramafic mantle with seismic velocity around 8 km/sec.

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Explain the Moho discontinuity on the basis of seismic evedenace ​

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Explain the Moho discontinuity on the basis of seismic evedenace