It is called the MohoroviÄić 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.
It is called the Mohorovi?i? 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 boundary between Earth's crust and mantle is called the Moho Discontinuity. 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.
This is rather unimaginatively entitled the Core Mantle boundary (CMB) by geophysicists. The base of the mantle is marked by a seismic discontinuity known as the Gutenberg discontinuity.
the boundary between mantel and crust is mohorovisic
the boundary between mantel and core is guttenberg
The Mohorovicic Discontinuity is the boundary between the crust and the mantle, where seismic waves change velocity.
The boundary between the crust and the upper mantle is called the Mohorovičić discontinuity, commonly known as the Moho.
It is between the Crust and the upper mantle
The crust is part of the lithosphere, so there is no boundary between them. There is a boundary between the crust and the other part of the lithosphere which is the uppermost mantle. It is called the Mohorovicic Discontinuity or the 'Moho' for short.
The upper mantle is in between the lower mantle and the earths crust Crust- the outer most solid shell of the earth. The Uppermost mantle and the earth's crust form the lithosphere.
The Mohorovicic Discontinuity is the boundary between the crust and the mantle, where seismic waves change velocity.
The boundary between the crust and the upper mantle is called the Mohorovičić discontinuity, commonly known as the Moho.
It is between the Crust and the upper mantle
The crust is part of the lithosphere, so there is no boundary between them. There is a boundary between the crust and the other part of the lithosphere which is the uppermost mantle. It is called the Mohorovicic Discontinuity or the 'Moho' for short.
The upper mantle is in between the lower mantle and the earths crust Crust- the outer most solid shell of the earth. The Uppermost mantle and the earth's crust form the lithosphere.
The mantle lies between the crust and the outer core of Earth's interior, and is not within the crust.
A distance of about 1,800 miles [2,896.8 kilometers] separates the earth's mantle from the earth's crust.
its called the mantle
It is the mantle.
"moho" is the plate boundary between earth's crust and the mantle.
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
The Croatian seismologist Andrija Mohorovicic.