Want this question answered?
mantle and crust
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
The mantle is that part of the Earth between the crust and the outer core. It's upper boundary is at the base of the crust at a depth below the surface which can vary between 7 and 35 km. It extends all the way to the Earth's outer core at a depth of around 2890 km.the Earths mantle is located between the crust and outer core of the Earth. it is the thickest layer.
As measured by its thickness from upper boundary to lower boundary in a downward direction, the mantle is the thickest layer of the Earth.
The mantle.
It is between the Crust and the upper mantle
"moho" is the plate boundary between earth's crust and the mantle.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
mantle and crust
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
The mantle is that part of the Earth between the crust and the outer core. It's upper boundary is at the base of the crust at a depth below the surface which can vary between 7 and 35 km. It extends all the way to the Earth's outer core at a depth of around 2890 km.the Earths mantle is located between the crust and outer core of the Earth. it is the thickest layer.
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 sometimes magnesium rich Mohorovičić discontinuity, which often is called simply 'Moho', forms the boundary between the basalt rich crust and the planet's underlying, iron rich mantle.
The Earth's interior is made up of four layers, the crust, mantle, outer core and the inner core. In the mantle, temperatures range between 500 to 900 degrees Celsius at the upper boundary with the crust; to over 4,000 degrees Celsius at the boundary with the outer core.
It is the boundary between the earth's crust and mantle, across which there is a sudden change in the velocity of seismic waves Often shortened to Moho
As measured by its thickness from upper boundary to lower boundary in a downward direction, the mantle is the thickest layer of the Earth.
In the mantle, temperatures range between 500 to 900 °C (932 to 1,652 °F) at the upper boundary with the crust; to over 4,000 °C (7,230 °F) near the boundary with the core.