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Who is the Yugoslavian scientist discovered separation between crust and mantle?
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
Who discovered 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.
Who discovered the boundary between the crust and the mantle?
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija Mohorovičić in 1909. This boundary is known as the Mohorovičić discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
Who discovered the crust mantle seismic discontinuity?
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, 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
What is named after the German geologist that discovered the thing that separates the earth's mantle from the outer core?
the Gutenberg discontinuity
Who discovered the mohorovicic?
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.
Boundary between earth's crust and mantle?
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.
How seismologists discovered that most of the mantle is solid?
Seismologists discovered that most of the Earth's mantle is solid by analyzing seismic wave data generated by earthquakes. When seismic waves travel through the Earth, their speed and behavior change depending on the material they pass through. The observation that primary (P) waves, which can travel through solids, move faster than secondary (S) waves, which can only travel through solids, indicated that the mantle is primarily solid. Additionally, the reflection and refraction patterns of these waves provided further evidence of the solid nature of the 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 the Outer Core?
The outer core of the Earth was indirectly discovered by detecting seismic waves that travel through it. Scientists used data from earthquakes and seismic waves to infer the existence and properties of the outer core, which lies beneath the mantle.
What is the name given to the top portion of the Earth's mantle?
The boundary between the crust and the mantle is called the Mohorovicic discontinuity. It is also called simply the Moho and it is the abrupt divide between faster and slower speeds where the mantle starts.
