The central part of the → Earth’s core, composed of solidified
→ iron and → nickel, and
extending from a depth of about 5100 km to the center of the Earth, at 6360 km.
Its radius is about 1/3 that of the whole core
and is effectively decoupled from the → mantle due to the
molten nature of the surrounding → outer core.
The radius of the inner core is defined by a small increase in
→ compressional wave velocity at a radius of about 1200 km.
Its density is about 12 g/cm3. The → temperature
of the inner core has been estimated at 5000-7000 °C.
See also: → inner; → core.