
mineral
Bornite (“peacock ore”), likely chalcopyrite-bearing sulfide specimen
Bornite, Cu₅FeS₄, commonly intergrown with chalcopyrite (CuFeS₂) and oxidized copper sulfides
AI-generated identification · may be incorrectMetallic to submetallic luster; dark bronze-brown fresh surfaces with iridescent purple, blue, green, and gold tarnish. Mohs hardness 3–3.25; opaque, massive, with poor cleavage and high specific gravity (~4.9–5.3).
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Physical properties
Metallic to submetallic luster; dark bronze-brown fresh surfaces with iridescent purple, blue, green, and gold tarnish. Mohs hardness 3–3.25; opaque, massive, with poor cleavage and high specific gravity (~4.9–5.3).
Formation & geological history
Forms in hydrothermal copper deposits, commonly replacing or filling veins in igneous and metamorphic host rocks; deposits range from Precambrian to modern geologic ages. The vivid colors develop through surface oxidation and tarnishing.
Uses & applications
Primarily an important copper ore; attractive pieces are sold as mineral specimens and occasionally used decoratively. It is generally unsuitable for jewelry because it is soft and tarnishes readily.
Geological facts
Bornite is nicknamed “peacock ore” for its multicolored oxidation film. Freshly broken bornite is typically copper-brown rather than intensely blue-purple.
Field identification & locations
Identify it by its heavy feel, metallic appearance, softness, and iridescent tarnish; a copper streak or chemical testing can help distinguish it from similarly colored chalcopyrite. Common localities include Cornwall, England; Butte, Montana; Mexico; Peru; and the Canadian Shield.
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