15g/cm3
between 12.6 and 13 g/cm3
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.
the inner part of earths core
15 g/cm3
15 g/cm3
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
No, the average density of Earth's Moon is about 3.3 g/cm^3, which is much lower than the average density of Earth's core. The core of the Earth is composed of mainly iron and nickel, giving it a much higher average density compared to the Moon.
Yes earths inner core is a dense ball of metal earths outer core is a layer of molten (melted) metal