
Mineral
Pyrite in Quartz
Iron Sulfide (FeS2) in Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6-6.5 (Pyrite), 7 (Quartz); Color: Brass-yellow metallic grains in tan/white matrix; Luster: Metallic (gold-like) and vitreous; Crystal system: Cubic/Isometric (Pyrite); Specific gravity: 4.9-5.2.
- Hardness
- 6-6
- Color
- Brass-yellow metallic grains in tan/white matrix
- Luster
- Metallic (gold-like) and vitreous
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Physical properties
Hardness: 6-6.5 (Pyrite), 7 (Quartz); Color: Brass-yellow metallic grains in tan/white matrix; Luster: Metallic (gold-like) and vitreous; Crystal system: Cubic/Isometric (Pyrite); Specific gravity: 4.9-5.2.
Formation & geological history
Formed in hydrothermal veins and through metamorphic processes where sulfur-rich fluids crystallize in fractures within host rocks, often associated with gold-bearing ores. Common in ancient mountain-building environments.
Uses & applications
Source of sulfur and sulfuric acid in industry; indicator mineral for gold prospecting; popular for student education and mineral collecting.
Geological facts
Commonly known as 'Fool's Gold' due to its resemblance to real gold. Unlike gold, which is soft and malleable, pyrite is brittle and leaves a greenish-black streak when rubbed on a porcelain plate.
Field identification & locations
Identify in the field by checking for metallic luster and cubic crystal habits; check hardness with a steel knife (pyrite is harder than gold). Frequently found in mining districts and sedimentary rock outcrops near metallic deposits.
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