
A terrestrial planet like Earth, whose sulfur content depends on its formation location and process.A rocky planet, also called a terrestrial planet, is a planet composed primarily of silicate rocks and metals, as opposed to gas giants like Jupiter or ice giants like Neptune. Earth, Venus, Mars, and Mercury are the rocky planets in our solar system. The seed definition highlights that the sulfur content of a rocky planet is not uniform but depends on where and how the planet formed, serving as a 'chemical fingerprint' of its birth environment.
The term 'terrestrial planet' dates back to ancient astronomy, but the modern understanding of their formation and composition emerged in the 20th century with the development of planetary science and the analysis of meteorites.
Rocky planets form in the inner regions of a protoplanetary disk, where temperatures are high enough for metals and silicates to condense into solid grains. These grains collide and stick together, gradually building up planetesimals and then planets. The sulfur content is determined by the local temperature and the availability of sulfur-bearing compounds, which vary with distance from the star. For instance, sulfur can be incorporated into the core or mantle depending on the oxidation state and the presence of iron, and later volcanic activity can release it into the atmosphere.
Understanding rocky planet composition is essential for interpreting exoplanet observations, such as those from the James Webb Space Telescope, which can infer atmospheric composition and surface properties of distant worlds.
Mercury, the smallest rocky planet, has an unusually large iron core, making up about 85% of its radius, which is thought to be the result of a giant impact that stripped away much of its rocky mantle.






















