Pyrite

3320
June 23, 2025, 10:30 AM
Guide
Highlights at a glance
Pyrite, known as "Fool's Gold," is an iron disulfide (FeS₂) mineral with a brassy yellow color and metallic luster. It crystallizes in the cubic system and commonly forms cubes, octahedrons, or spherical framboidal aggregates. With a Mohs hardness of 6–6.5 and specific gravity of 4.95–5.10, pyrite has a greenish- to brownish-black streak and exhibits conchoidal fracture. Chemically, it contains 46.6% iron and 53.4% sulfur, oxidizing in moist air to produce iron hydroxides and sulfuric acid—contributing to acid mine drainage. It decomposes upon heating and dissolves in nitric acid but not in hydrochloric acid. Found in various geological settings, pyrite occurs as massive, disseminated, or framboidal forms and is associated with sulfide minerals like chalcopyrite and galena, as well as gangue minerals such as quartz and calcite. It often hosts trace elements including gold, silver, arsenic, and nickel, making it economically significant despite its deceptive appearance.
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