It is estimated to be between 10.0-12.3 g/cm3.
681 g/km5
its 657.89
Gutenburg Discontinuity
There are several layers between the outer core and the crust mainly combined into one and called the Mantle.
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
Gutenburg Discontinuity
Crust Mantle Core Inner Core
Gutenburg Discontinuity
The D'' area of the mantle extends from 2798 km to 2900 km, which is the boundary between the mantle and the liquid outer core. At this level, the pressures are enormous, roughly equal to 1.4 million units of atmospheric pressure.
There are differences in chemistry (the mantle is mainly ultramafic rock--the outer core is metallic), in phase (the mantle is predominately solid--the outer core is liquid), in depth (the outer core is closer to the center of the Earth), and in density (the outer core is more dense).
The outer core.
The outer core.
There are several layers between the outer core and the crust mainly combined into one and called the Mantle.
Between the outer core and the crust.
the outer core :)
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The relationship between the inner core outer core-mantle lithosphere and asthenosphere is that the coolest layers are farthest from the core.
Between the inner core and lowwer mantle.
Gutenburg Discontinuity