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The immense pressure from the layers outside of the inner core.
The amount of pressure overcomes the material's disposition to melting at high temperature. It solidifies.
Convection from the inner layers of the earth
Crust Mantle Outer Core Inner Core
it remains solid because of all the pressure. Also, it is solid because it is the inner core
The immense pressure from the layers outside of the inner core.
The amount of pressure overcomes the material's disposition to melting at high temperature. It solidifies.
The inner core.
Crust, mantle, and inner core.
Convection from the inner layers of the earth
asthenosphere outer core inner core and crust
Crust, Mantle, Inner Layer, Outer Layer
Outer Core, Inner Core, Mantle, Crust
Crust Mantle Outer Core Inner Core
the crust the mantle the outer core and the inner core.
It's because of the pressure from the layers above causes the particles of iron and nickel to be tightly packed.
Inner core (probably solid); outer core (probably liquid); mantle, crust.