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.
Andrija Mohorovičić was from Croatia. He was a Croatian meteorologist and seismologist known for discovering the boundary between the Earth's crust and mantle, now named the Mohorovičić discontinuity in his honor.
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.
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
Andrija Mohorovičić, a Croatian seismologist, discovered the Mohorovičić discontinuity in 1909. This boundary separates the Earth's crust from the underlying mantle and is marked by a change in seismic wave velocities.
He was old and sick.
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.
Four sons, named Andrija, Ivan, Stjepan and Franjo.
Andrija Mohorovicic, a Croatian seismologist, discovered the Mohorovicic discontinuity in 1909. This boundary between the Earth's crust and mantle was named in his honor.
Andrija Mohorovičić was from Croatia. He was a Croatian meteorologist and seismologist known for discovering the boundary between the Earth's crust and mantle, now named the Mohorovičić discontinuity in his honor.
Andrija_Mohorovičić, a Croatian seismologist (1857-1936), first theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho). The layer was identified by changes in the propagation of waves generated by seismic events.
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
The project was suggested in March 1957 by Walter Munk, a NAS member (1956) and member of the National Science Foundation (NSF) Earth Science Panel. Andrija Mohorovicic a Croatian geologist discovered that there was an area, known as the "moho". The Moho was named for Andrija Mohorovicic, who first proposed the existence of such a discontinuity.
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.
No. The Mohorovicic Discontinuity (Moho) is the dividing line between the crust and the mantle, deep within the Earth. The approximate temperature there is 600°C (1112 °F). It is named for seismologist Andrija Mohorovičić (1857-1936).
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
Andrija Mohorovičić, a Croatian seismologist, discovered the Mohorovičić discontinuity in 1909. This boundary separates the Earth's crust from the underlying mantle and is marked by a change in seismic wave velocities.