The outer and inner core.
The Moho separates the crust and the mantle.
discontinuity
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.
Crust
The Gutenberg discontinuity is found directly above the outer core.
The crust and mantle.
The Moho separates the crust and the mantle.
lower mantle from upper core
mohorocivic discontinuity or moho
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
discontinuity
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.
Crust
The Gutenberg discontinuity is found directly above the outer core.
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
The distinction of the solid inner core from the liquid outer core of Earth was discovered in 1936 by Inge Lehmann. Inge Lehmann is a seismologist.
The inner core has a radius of 1220 kmA extending from the centre of the Earth approximately 6370 km below Earth's surface to 5150 km below the surface (the change from inner to outer core is marked by a density change known as the Lehmann discontinuity). The inner core has a total volume of 7.4207x109 km3.