The MohoroviÄić Discontinuity, also called the Moho Discontinuity, was named for Andrija MohoroviÄić, the Croatian seismologist who first identified it in 1909.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
The Moho separates the crust and the mantle.
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.
"moho" is the plate boundary between earth's crust and the mantle.
The Moho discontinuity is 31 miles/50KM thick.
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
moho
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.
The Moho separates the crust and the mantle.
The sometimes magnesium rich Mohorovičić discontinuity, which often is called simply 'Moho', forms the boundary between the basalt rich crust and the planet's underlying, iron rich mantle.
The Mohorovičić discontinuity, also known as the Moho, marks the boundary between the Earth's crust and mantle. It is identified by a sudden increase in seismic wave velocities, indicating a change in rock density and composition at this boundary.
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 Mohorovičić discontinuity (Moho) separates the Earth's crust from the underlying mantle. It is found beneath continents and beneath ocean basins.
"moho" is the plate boundary between earth's crust and the mantle.