The different earth layers have different density cores. For instance, the continental crust varies between 2. 7 and 3. 0, the oceanic crust between 3. 0 and 3. 3, the mantle 3. 3 to about 5. 7, the outer core 9. 9 to 12. 2, while the inner core is between 12. 6 to 13. 0.
How is Mercury's density is about high as the earths density
15g/cm3
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.
Earth's average density is about 5.52 grams per cubic centimeter. This density is determined by the distribution of material in Earth's layers, with the denser iron-nickel core contributing to the overall value. Earth's density is higher than that of most other planets in our solar system.
Changes in climate
The average density of the Earth's outer core is estimated to be around 10-12 grams per cubic centimeter. This high density is mainly due to the presence of iron and nickel in the outer core, which are heavy elements.
How do changes in heat energy affect the density of earths mantle material
The earths outer core's most abundant elemant is silicon. :)
POP DENSITY
Well, some planets, such as Mercury, have little density. For example, the amount of density in oil compared to water. That scenario is an example of the amount of density that you might expect on such planets as Venus.
The Earth's crust is the thinnest layer, ranging from about 5-70 km thick. The average density of the Earth's crust is around 2.7-3.0 g/cm³.
The Earth's core.