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To the best of my knowledge, he was a Croatian geologist the developed the theory of discontinuity, which means that the crust of the Earth is about 6 miles thick under the oceans and about 22 miles thick under the continents.

Now called 'Moho's Discontinuity' or simply 'Moho'

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13y ago

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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.


Who discovered mohorovicic distensity?

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


mohorovicic discontinuity?

interface between the crust and the upper mantle


How did Andriza Mohorovicic discover moho?

Andrija Mohorovicic discovered the Moho boundary, or Mohorovicic discontinuity, in 1909 by observing the travel times of seismic waves. He noticed a sudden increase in seismic wave velocity at a certain depth in the Earth's interior, which indicated a change in composition and density between the Earth's crust and mantle. This boundary was later named after Mohorovicic in recognition of his discovery.


Where does the Mohorovicic discontinuity occur?

Crust and Mantle.


How did andrija mohorovicic die?

He was old and sick.


The mohorovicic discontinuity occur between the crust and the?

mantle


What is the boundary between the mantle and outercore?

the Mohorovicic Discontinuity


What is the region where the lithosphere meet the mantle?

The Mohorovicic Discontinuity.


What is the region where lithosphere meets the mantle?

The Mohorovicic Discontinuity.


Who was 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).


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).