
mineral
Chalcopyrite (Peacock Ore)
Chalcopyrite (CuFeS2)
AI-generated identification · may be incorrectHardness: 3.5-4 (Mohs); Color: Brassy yellow naturally, but often exhibits colorful iridescent tarnish (purple, blue, green, gold); Luster: Metallic; Crystal Structure: Tetragonal; Cleavage: Poor; Specific Gravity: 4.1-4.3
- Hardness
- 3
- Luster
- Metallic
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Physical properties
Hardness: 3.5-4 (Mohs); Color: Brassy yellow naturally, but often exhibits colorful iridescent tarnish (purple, blue, green, gold); Luster: Metallic; Crystal Structure: Tetragonal; Cleavage: Poor; Specific Gravity: 4.1-4.3
Formation & geological history
Formed in hydrothermal veins, contact metamorphic deposits, and as a primary mineral in igneous rocks. When the surface oxidizes, it creates the characteristic iridescent tarnish known as bornite or peacock ore coating.
Uses & applications
The most important ore of copper; also used as a decorative specimen for collectors and occasionally in metaphysical jewelry.
Geological facts
While often confused with gold, it is more brittle and has a lower hardness. The iridescent effect is most commonly produced or enhanced by acid washing the mineral in a laboratory to display the range of colors seen here.
Field identification & locations
Identified by its metallic luster, brassy base color (where fresh), and greenish-black streak. Commonly found in copper mines worldwide, particularly in Arizona, Chile, and Cornwall. Collectors should look for vibrant multi-colored oxidation layers.
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