Planets, excluding gas giants and water worlds, are primarily composed of silicon, iron, and carbon, but they can also contain a variety of other elements based on the metallicity of the primordial gas cloud from which they formed. The composition of planets is influenced by their proximity to their parent star, with inner planets being denser and richer in metals due to the loss of volatile elements. It is statistically improbable for a planet to be formed from a single element, as the gas cloud is a mixture of various elements that coalesce under gravity. The classification of planets as silicate, iron, or carbon refers to their predominant materials rather than their exclusive composition. Overall, planets are expected to be mixtures of elements, reflecting the abundance of materials found in the universe.