epSmithite

EpSmithite is a fictional mineral with the chemical formula Fe3S2. It is a dark gray metallic solid with a Mohs hardness of 4.5 and a specific gravity of 5.8. EpSmithite is found in association with iron and sulfur deposits, often in igneous and metamorphic environments. Its crystalline structure is monoclinic, and it typically forms in granular masses or as small prismatic crystals.

The mineral was first described in 1972 by Dr. Evelyn P. Smith, a geologist specializing in mineralogy, after its discovery in a meteorite fragment found in Antarctica. Its name honors her contributions to the field. While epSmithite has not been found in significant quantities for commercial use, it is of interest to mineralogists and geochemists studying the formation of iron-sulfur compounds under extreme conditions.

Research into epSmithite has focused on its unique crystal structure and its potential role in extraterrestrial geological processes. Its presence in meteorites suggests it may form under high-pressure, high-temperature conditions not commonly found on Earth's surface. Further studies are ongoing to understand its formation mechanisms and potential occurrence in other celestial bodies.