
mineral
Tumbled metallic sulfide mineral, likely pyrite
Pyrite (FeS₂), tentatively; possibly marcasite or a pyrite-rich nodule
AI-generated identification · may be incorrectSmall rounded specimen with metallic gray-brassy luster and granular/crystalline texture. Pyrite hardness is 6–6.5 Mohs, cubic crystal system, brittle, with no prominent cleavage and specific gravity about 5.0; the image is insufficient for confident identification.
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Physical properties
Small rounded specimen with metallic gray-brassy luster and granular/crystalline texture. Pyrite hardness is 6–6.5 Mohs, cubic crystal system, brittle, with no prominent cleavage and specific gravity about 5.0; the image is insufficient for confident identification.
Formation & geological history
Likely formed hydrothermally or in sedimentary environments through sulfide mineral precipitation; pyrite ranges from Precambrian to modern geological settings. Marcasite is chemically identical but orthorhombic and less stable.
Uses & applications
Collected as a mineral specimen and occasionally used as a sulfur source; pyrite is sometimes cut as a novelty gemstone, while sulfide ores can be economically important for associated metals.
Geological facts
Pyrite is commonly called “fool’s gold,” but its darker metallic appearance here is not diagnostic. A streak test, hardness test, density, and crystal-form examination would distinguish it from galena, hematite, and marcasite.
Field identification & locations
Common in hydrothermal veins, coal beds, shales, and sedimentary rocks worldwide, especially Peru, Spain, Italy, and the United States. Pyrite leaves a greenish-black streak and typically scratches glass; avoid prolonged moisture, which can cause deterioration.
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