Rock Identifier
Tumbled polymetallic mineral specimen, likely chalcopyrite-bearing ore (Probable chalcopyrite (CuFeS₂) with quartz and iron-oxide minerals; exact identification is uncertain from the photograph) — mineral
mineral

Tumbled polymetallic mineral specimen, likely chalcopyrite-bearing ore

Probable chalcopyrite (CuFeS₂) with quartz and iron-oxide minerals; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Brassy bronze to coppery metallic patches occur in a dark matrix with pale quartz-like areas. Chalcopyrite has Mohs hardness 3.5–4, metallic luster, tetragonal crystals, poor cleavage, and specific gravity about 4.1–4.3; tarnish may create blue, purple, or brown colors.

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Physical properties

Brassy bronze to coppery metallic patches occur in a dark matrix with pale quartz-like areas. Chalcopyrite has Mohs hardness 3.5–4, metallic luster, tetragonal crystals, poor cleavage, and specific gravity about 4.1–4.3; tarnish may create blue, purple, or brown colors.

Formation & geological history

Likely hydrothermal sulfide ore formed in veins or massive sulfide deposits during cooling of mineral-rich fluids; age depends on locality and cannot be determined visually.

Uses & applications

Copper ore and a popular mineral-collecting material; polished pieces are used decoratively, but this is generally not a gemstone or construction stone.

Geological facts

Chalcopyrite is commonly called “peacock ore” when artificially or naturally iridescent, though the visible colors may also reflect surface oxidation or coatings.

Field identification & locations

Look for metallic brassy color, high density, and a dark sulfide matrix; a streak, hardness, magnetism, and chemical tests would help distinguish chalcopyrite from bornite or metallic slag. Common worldwide in copper deposits.