Rock Identifier
Copper-bearing rock, likely bornite/chalcopyrite in iron-rich matrix (Chalcopyrite (CuFeS₂) and/or bornite (Cu₅FeS₄) in limonite/goethite matrix) — mineral
mineral

Copper-bearing rock, likely bornite/chalcopyrite in iron-rich matrix

Chalcopyrite (CuFeS₂) and/or bornite (Cu₅FeS₄) in limonite/goethite matrix

AI-generated identification · may be incorrect

Metallic brassy-gold to bronze sulfide patches occur in a dark red-brown, earthy iron-oxide matrix; sulfides are typically Mohs 3.5–4, with indistinct cleavage and metallic luster, while the matrix is softer and dull. The apparent green-blue coating may be copper oxidation products such as malachite or chrysocolla.

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Physical properties

Metallic brassy-gold to bronze sulfide patches occur in a dark red-brown, earthy iron-oxide matrix; sulfides are typically Mohs 3.5–4, with indistinct cleavage and metallic luster, while the matrix is softer and dull. The apparent green-blue coating may be copper oxidation products such as malachite or chrysocolla.

Formation & geological history

Formed in hydrothermal copper-ore veins or disseminated deposits, commonly by sulfide mineralization followed by near-surface oxidation; age depends on locality and cannot be determined from the image.

Uses & applications

Primarily an ore and teaching/collecting specimen; chalcopyrite is a major copper source, while attractive pieces may be sold as mineral specimens rather than used as gemstones.

Geological facts

Bornite is called “peacock ore” when iridescent; copper sulfides can tarnish to blue, green, purple, or bronze colors, though artificial peacock ore is also common.

Field identification & locations

Look for brassy metallic grains, dark streak, moderate heft, and possible green copper staining; confirm with streak, hardness, specific gravity, and ideally chemical or X-ray testing. Common in copper districts worldwide, including Arizona, Montana, Peru, and Cornwall.