Rock Identifier
Copper-bearing quartz/rock fragment with attached mica (Chalcopyrite-bearing quartz or altered igneous rock; attached flake likely muscovite or biotite mica) — mineral
mineral

Copper-bearing quartz/rock fragment with attached mica

Chalcopyrite-bearing quartz or altered igneous rock; attached flake likely muscovite or biotite mica

AI-generated identification · may be incorrect

Metallic brassy-gold and blue-green tarnish suggests chalcopyrite, with quartz or feldspar matrix and a strongly reflective mica flake. Chalcopyrite hardness is 3.5–4, metallic luster, imperfect cleavage, and specific gravity about 4.1–4.3; identification is uncertain from the image alone.

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Physical properties

Metallic brassy-gold and blue-green tarnish suggests chalcopyrite, with quartz or feldspar matrix and a strongly reflective mica flake. Chalcopyrite hardness is 3.5–4, metallic luster, imperfect cleavage, and specific gravity about 4.1–4.3; identification is uncertain from the image alone.

Formation & geological history

Likely formed in hydrothermal veins or altered igneous rocks, where copper sulfides crystallized from hot fluids; the specimen’s geological age cannot be determined visually. Surface oxidation produces blue-green copper sulfates and related tarnish minerals.

Uses & applications

Copper sulfide minerals are mined for copper; attractive pieces are collected, while mica has industrial uses in electrical insulation and fillers. This small natural specimen has modest decorative value.

Geological facts

Chalcopyrite is commonly called “peacock ore” when its iridescent tarnish is prominent, though artificially treated pieces are also sold under that name.

Field identification & locations

Look for brassy metallic grains, iridescent blue-purple oxidation, and a dark or pale matrix; a streak test, hardness test, and copper-mineral testing would help confirm it. Common localities include Peru, Mexico, Arizona, Montana, and Cornwall.