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Where is the Moho locate?

The Moho, or Mohorovicic Discontinuity, is the boundary 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


Moho is another word for what?

The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.


It separates the mantle and the crust?

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.


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

Mohorovicic discontinuity (or simply Moho)


Which feature of earth was discovered by studying the velocities of the seismic waves?

the Mohorovicic (Moho) discontinuity


Is the Outer Core known as the Moho?

No, the Outer Core is not known as the Moho. The Moho, short for Mohorovicic Discontinuity, is the boundary between the Earth's crust and mantle, while the Outer Core is a layer of molten iron and nickel that surrounds the Earth's solid inner core.


What separate the crust from the mantle?

The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.


Who was Andrija Mohorovicic?

Andrija_Mohorovičić (1857-1936) was a Croatian seismologist and meteorologist who theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho).


The Moho barrier is the dividing line between the crust and the mantle?

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.


Does the Moho barrier separate the earth's crust and mantle?

Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.