
mineral
Pyrite in Quartz
Iron Disulfide (FeS2) in Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6-6.5 (Pyrite) / 7 (Quartz); Color: Brass-yellow (metallics), white to grey (matrix); Luster: Metallic to vitreous; Crystal Structure: Isometric/Cubic (Pyrite), Trigonal (Quartz); Specific Gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Brass-yellow (metallics), white to grey (matrix)
- Luster
- Metallic to vitreous
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Physical properties
Hardness: 6-6.5 (Pyrite) / 7 (Quartz); Color: Brass-yellow (metallics), white to grey (matrix); Luster: Metallic to vitreous; Crystal Structure: Isometric/Cubic (Pyrite), Trigonal (Quartz); Specific Gravity: 4.9-5.2.
Formation & geological history
Formed in hydrothermal veins and sedimentary environments through the precipitation of iron-rich fluids in the presence of sulfur. Often found in metamorphic rocks and associated with gold deposits.
Uses & applications
Primarily used as an ore of sulfur and for the production of sulfuric acid; used in jewelry as 'marcasite' and highly valued as a collector's specimen.
Geological facts
Pyrite is famously known as 'Fool's Gold' because its color and luster often deceive novice prospectors, although it is much harder and more brittle than real gold.
Field identification & locations
Identify by its brassy color, cubic crystal habit, and blackish-green streak. Common in mines worldwide, particularly in Peru, Spain, and the USA. Collectors look for well-defined cubes or pyritohedrons.
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