The crust and mantle.
The Moho discontinuity is 31 miles/50KM thick.
the Mohorovicic (Moho) discontinuity
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
It is called the Mohorovicic Discontinuity, or the Moho for short.
moho
The Moho separates the crust and the mantle.
mohorocivic discontinuity or moho
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.moho
The Moho discontinuity is 31 miles/50KM thick.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
the Mohorovicic (Moho) discontinuity
the Mohorovicic (Moho) discontinuity
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
It is called the Mohorovicic Discontinuity, or the Moho for short.
moho
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.