
mineral
Bornite (Peacock Ore)
Bornite (Cu5FeS4)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Bronze-brown but tarnishes to iridescent blue/purple/green; Luster: Metallic; Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 5.06-5.08
- Hardness
- 3 on Mohs scale
- Color
- Bronze-brown but tarnishes to iridescent blue/purple/green
- Luster
- Metallic
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Physical properties
Hardness: 3 on Mohs scale; Color: Bronze-brown but tarnishes to iridescent blue/purple/green; Luster: Metallic; Crystal structure: Orthorhombic; Cleavage: Poor; Specific gravity: 5.06-5.08
Formation & geological history
Forms primarily in hydrothermal veins and as a primary or secondary copper mineral in porphyry copper deposits. It is often found in contact metamorphic rocks and basic igneous rocks.
Uses & applications
Significant ore of copper; highly popular as a collector's specimen due to its vibrant 'peacock' iridescence.
Geological facts
Commonly known as 'Peacock Ore' because of its rainbow-like tarnish. While bornite naturally tarnishes, many samples sold in gift shops are actually chalcopyrite that has been acid-washed to force the iridescent oxidation.
Field identification & locations
Identify by its iridescent metallic tarnish and high copper content. Commonly found in copper mining districts like those in Chile, Arizona (USA), and Cornwall (UK). Submerging a suspect piece in dilute acid to see if it turns bright colors is a common test for artificial enhancement.
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