The average specific gravity of Earth is about 5.52.
Here's why:
* Specific gravity is the ratio of the density of a substance to the density of a reference substance, usually water.
* Earth is composed of a dense iron core, a less dense mantle, and a relatively thin crust.
* The varying densities of these layers contribute to the overall average specific gravity.
Important Note:
* The specific gravity of different parts of Earth varies significantly. The core has a much higher specific gravity than the crust.
* The figure of 5.52 is an average, and it doesn't account for regional differences.