the Mohorovicic Discontinuity
hot spots begin at the boundary between the mantle and the outercore.
The boundary of mantle and core are called Gutenberg Discontinuity
The boundary between the mantle and core is called the core-mantle boundary. This region is marked by a significant change in density and composition, representing the transition from the solid mantle to the liquid outer core of the Earth.
Crust,Mantle,Outercore,and inner core.
Crust,Mantle,Outercore,and inner core.
Crust,Mantle,Outercore,and inner core.
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
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.
The mantle is below the plates.
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
"moho" is the plate boundary between earth's crust and the mantle.
4 the crust, mantle ,inncore,outercore 5