Zeme

Maidla Mingito Nepneu Maganlis Therumlon Tharopto
 * Maidla is a terrestrial planet with a light atmosphere of carbon dioxide and hydrogen sulfide. The surface is hot, and mainly composed of magnesia with deposits of sulfur. Over a dozen volcanoes are erupting across the surface.
 * Mingito is a sunbaked wasteland of sodium, chlorates, and radioactives. Its relatively light mass has left it tidally locked to Zeme, with a day side "hot pole" and a night side "cold pole". The powerful solar wind has stripped most of the atmosphere away.
 * With a rare combination of features, Nepneu is of particular interest to the scientific community. Nepneu is a small terrestrial planet, with a thin atmosphere of carbon dioxide and krypton. It’s surface is scorching hot. The crust mainly consists of silicates laced with iron.
 * Maganlis is a rock terrestrial with an atmosphere of sulphur dioxide and trace amounts of helium. Scans reveal ancient lava plains on the surface, implying a geologically active past. The crust consists of sulphur and basalts, but the planet's mass suggests a core of iron and heavier materials.
 * Therumlon is a frigid world with a thick nitrogen-argon atmosphere. The crust contains silicates and unremarkable ores, but is surprisingly rich in phosphates. Since the atmosphere lacks free oxygen, the phosphates are relatively pure.
 * Tharopto is a typical hydrogen-helium gas giant with traces of chlorine and sulphur in its atmosphere.