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Andrija Mohorovičić, a Croatian seismologist, is best known for discovering the Mohorovičić discontinuity, commonly referred to as the "Moho." This boundary marks the transition between the Earth's crust and the underlying mantle, characterized by a significant change in seismic wave velocities. His discovery, made in 1909, was pivotal in advancing the understanding of Earth's internal structure and has had a lasting impact on the field of geology and seismology.
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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.
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).
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.
mohorovicic discontinuity?
interface between the crust and the upper mantle
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
Who discovered mohorovicic distensity?
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the 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.
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).
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.
mohorovicic discontinuity?
interface between the crust and the upper mantle
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).
