
mineral
Pyrite in Quartz
Iron Sulfide (FeS2) in Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (for quartz, pyrite is 6-6.5); Color: Brass-yellow metallic flecks in a whitish/grayish translucent base; Luster: Metallic for pyrite, vitreous for quartz; Crystal Structure: Isometric for pyrite, trigonal for quartz; Specific Gravity: ~2.65 for quartz, ~5.0 for pyrite
- Hardness
- 6-7 on Mohs scale (for quartz, pyrite is 6-6
- Luster
- Metallic for pyrite, vitreous for quartz
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Physical properties
Hardness: 6-7 on Mohs scale (for quartz, pyrite is 6-6.5); Color: Brass-yellow metallic flecks in a whitish/grayish translucent base; Luster: Metallic for pyrite, vitreous for quartz; Crystal Structure: Isometric for pyrite, trigonal for quartz; Specific Gravity: ~2.65 for quartz, ~5.0 for pyrite
Formation & geological history
Formed through hydrothermal vein systems where hot mineral-rich fluids deposit quartz and pyrite into surrounding rock fractures.
Uses & applications
Used primarily as mineral specimens for collectors, educational purposes, and occasionally in metaphysical practices.
Geological facts
Pyrite is commonly known as 'Fool's Gold' due to its brassy metallic sheen which has frequently tricked prospectors into thinking they found actual gold.
Field identification & locations
Easily identified by its distinctive metallic brass-yellow cubic or granular flecks embedded within a hard crystalline quartz matrix. Found globally in metalliferous veins and sedimentary deposits.
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