
mineral
Peacock Ore
Bornite (Cu5FeS4) or iridescent Chalcopyrite (CuFeS2)
AI-generated identification · may be incorrectHardness: 3-3.5 on Mohs scale; Color: Copper-red/brown on fresh surface, tarnishing to iridescent purple, blue, and gold; Luster: Metallic; Crystal Structure: Orthorhombic/Tetragonal; Cleavage: Poor/Invisible.
- Hardness
- 3-3
- Luster
- Metallic
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Physical properties
Hardness: 3-3.5 on Mohs scale; Color: Copper-red/brown on fresh surface, tarnishing to iridescent purple, blue, and gold; Luster: Metallic; Crystal Structure: Orthorhombic/Tetragonal; Cleavage: Poor/Invisible.
Formation & geological history
Formed in hydrothermal veins, contact metamorphic zones, and igneous intrusions. It is typically a primary copper mineral associated with other sulfides like pyrite and chalcocite.
Uses & applications
Primarily used as a major copper ore in the mining industry. Because of its brilliant iridescence, it is highly popular for decorative jewelry, metaphysical collections, and educational specimens.
Geological facts
The name 'Peacock Ore' is commonly used for both Bornite and acid-treated Chalcopyrite. While Bornite tarnishes naturally, many specimens sold in shops are Chalcopyrite that has been washed in acid to induce the rainbow colors.
Field identification & locations
Identify in the field by its metallic luster and the 'oil slick' rainbow tarnish. Unlike true gold, it has a greenish-black streak and is much more brittle. Common locations include Mexico, USA, and Chile.
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