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mohorovicic discontinuity?

interface between the crust and the upper mantle


The mohorovicic discontinuity occur between the crust and the?

mantle


Who discovered mohorovicic distensity?

Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle


Where did mohorovicic discontinuity get its name?

The Mohorovicic discontinuity is named after Croatian seismologist Andrija Mohorovicic, who first discovered it in 1909. It marks the boundary between the Earth's crust and the mantle and is characterized by a sudden increase in seismic wave velocity.


Where is the Moho locate?

The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.


Where does the Mohorovicic discontinuity occur?

Crust and Mantle.


What do you call the plastic zone between the mantle and the crust?

Mohorovicic discontinuity (or simply Moho)


What is the difference between Mohorovicic discontinuity and Gutenberg discontinuity?

Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.


Which layer of earth contains the mohorovicic discontinuity?

The Mohorovicic discontinuity is located at the boundary between the Earth's crust and mantle. It marks a change in seismic wave speeds, indicating a transition from the solid crust to the denser, semi-solid mantle below.


Who is the discoverer of mohorovicic discontinuity?

Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer


The seismic discontinuity at the base of the crust is known as?

The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.


Who is the Yugoslavian scientist discovered separation between crust and mantle?

The boundary between the crust and mantle is called the Mohorovicic discontinuity (or Moho); it is named in honor of the man who discovered it, the Croatian scientist Andrija Mohorovicic