
mineral
Dark sulfide-bearing mineral specimen, possibly bornite or chalcopyrite
Likely chalcopyrite (CuFeS₂) or bornite (Cu₅FeS₄), with pale quartz or carbonate coating
AI-generated identification · may be incorrectMetallic to submetallic luster, dark gray-black body with brassy golden patches; likely hardness about 3–4 Mohs and relatively high specific gravity. The close-up and reflective packaging obscure crystal form and cleavage, so identification is provisional.
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Physical properties
Metallic to submetallic luster, dark gray-black body with brassy golden patches; likely hardness about 3–4 Mohs and relatively high specific gravity. The close-up and reflective packaging obscure crystal form and cleavage, so identification is provisional.
Formation & geological history
Copper sulfide minerals commonly form in hydrothermal veins and disseminated ore deposits, often with quartz, calcite, or other sulfides; ages range from Precambrian to recent geological systems.
Uses & applications
Primarily mined as copper ore; attractive iridescent or brassy specimens are collected, but this piece appears to be an unexceptional small ore specimen rather than jewelry material.
Geological facts
Bornite is nicknamed “peacock ore” when tarnished with purple-blue colors; chalcopyrite commonly has a brass-yellow color and may tarnish iridescently.
Field identification & locations
Test for a brassy streak, metallic luster, and softness relative to a steel blade; chalcopyrite is commonly softer than quartz and may show green-black tarnish. Common localities include Arizona, Montana, Peru, Chile, Mexico, and Cornwall.
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