Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho
Moho is the boundery between the crust and the mantle
The mantle was not discovered by a single individual, but its composition and properties were studied and understood through the work of multiple scientists over time. Scientists such as Alfred Wegener, Arthur Holmes, and Inge Lehmann made significant contributions to our understanding of the Earth's mantle.
The Mohorovicic discontinuity occurs between the Earth's crust and the mantle. It marks the boundary where seismic waves change speed, indicating a change in the composition of the Earth's layers.
It is called the Mohorovičić discontinuity or the Moho for short.It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.
The Mohorovicic discontinuity is located at the boundary between the Earth's crust and mantle. It marks a change in seismic wave speeds, indicating a transition from the solid crust to the denser, semi-solid mantle below.
The boundary between the mantle and core was discovered by a seismologist named Inge Lehmann in 1936. She observed a reflection of seismic waves off this boundary, later named the "Lehmann discontinuity," which helped confirm the Earth's core-mantle structure.
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.
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 Mohorovicic (Moho) discontinuity
yo mamma so hairy,when i first saw her i thought its a gorilla.
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 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.
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).
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.
interface between the crust and the upper mantle
The discovery of moho was through seismic waves...There are two 2 waves namely, Primary and Secondary waves...Secondary waves cannot pass through liquid and gasses. Thus, There is an abrupt increase in the velocity of earthquake waves (specifically P- waves) at this point.
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.
He was old and sick.