
mineral
Native copper-bearing sulfide specimen
Likely chalcopyrite (CuFeS₂), possibly with native copper and iron oxides
AI-generated identification · may be incorrectMetallic luster with brassy, silver-gray, and reddish-orange tarnish; likely Mohs hardness 3.5–4, opaque, massive to granular, with indistinct cleavage. The reddish coating may be copper or oxidation products rather than intrinsic color.
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Physical properties
Metallic luster with brassy, silver-gray, and reddish-orange tarnish; likely Mohs hardness 3.5–4, opaque, massive to granular, with indistinct cleavage. The reddish coating may be copper or oxidation products rather than intrinsic color.
Formation & geological history
Forms in hydrothermal copper deposits, commonly in veins and disseminated ore; mineralization ranges from Precambrian to geologically recent. Exact identification and age require testing or locality information.
Uses & applications
Copper sulfide ores are mined for copper; attractive iridescent pieces are collected, though this small specimen has limited jewelry use and is not suitable for construction.
Geological facts
Chalcopyrite commonly develops blue, purple, or reddish “peacock ore” tarnish. A streak test, hardness test, and specific-gravity measurement can distinguish it from bornite, copper metal, and metallic slag.
Field identification & locations
Common localities include Chile, Peru, Mexico, the United States, Canada, and Australia. Confirm with a dark greenish-black streak, moderate hardness, and lack of strong malleability; an acid or laboratory test can verify copper minerals.
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