15g/cm3
15g/cm3
between 12.6 and 13 g/cm3
the inner part of earths core
The layers of Earth's interior from least to greatest density are: Crust Mantle Outer core Inner core
The Earth's compositional layers in order of increasing density are the crust, mantle, outer core, and inner core. The crust is the least dense layer, while the inner core is the most dense layer.
The radious of the inner core is 1,220km(760miles).
The inner core has the most or highest amount of density (iron/nickel).
The inner core Is solid and the outer core in liquid
The inner core was discovered in 1936 by Inge Lehmann and is generally believed to be composed primarily of iron and some nickel. Its estimated density is between 12.6 to 13.0 grams to cubic centimeters.
Yes earths inner core is a dense ball of metal earths outer core is a layer of molten (melted) metal
The immense pressure from the layers outside of the inner core.
iron and nickel is the answer and so is the inner core. the inner and the outer and together but the outer core is liquid and the inner core is solid