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The Mohorovičić discontinuity, also known as the Moho, is the boundary between the Earth's crust and the underlying mantle. It is characterized by a sudden increase in seismic wave velocities, indicating a change in the composition and density of the Earth's layers. The Moho typically lies at depths ranging from 5 to 70 kilometers beneath the Earth's surface.
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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.
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.
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).
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
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.
How did andrija mohorovicic die?
He was old and sick.
Where does the Mohorovicic discontinuity occur?
Crust and Mantle.
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).
