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.
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
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.
The crust and upper mantle make up the earth.
It is between the Crust and the upper mantle
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.
a mantle is something between the crust
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.
Crust and the upper mantle
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
moho
It is between the Crust and the upper mantle
moho
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.
The upper mantle is located beneath the Earth's crust, extending from about 30 to 400 kilometers deep. It is part of the Earth's mantle layer, which lies between the crust and the core.
The crust thins and thickens over the surface of the earth. At a mid-ocean ridge spreading center, the mantle is essentially at the surface. Under neath the Himalayan mountains it is well over 40km.