Rock Identifier
Weathered metallic sulfide-bearing rock, possibly chalcopyrite ore (Likely chalcopyrite (CuFeS₂) in a weathered host rock; identification is uncertain from the photograph) — mineral
mineral

Weathered metallic sulfide-bearing rock, possibly chalcopyrite ore

Likely chalcopyrite (CuFeS₂) in a weathered host rock; identification is uncertain from the photograph

AI-generated identification · may be incorrect

Brassy bronze-gold metallic patches occur in a dark gray, granular matrix with rusty oxidation. Chalcopyrite has Mohs hardness 3.5–4, metallic luster, tetragonal crystals, and poor cleavage; the specimen appears heavily weathered and may include iron oxides.

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Physical properties

Brassy bronze-gold metallic patches occur in a dark gray, granular matrix with rusty oxidation. Chalcopyrite has Mohs hardness 3.5–4, metallic luster, tetragonal crystals, and poor cleavage; the specimen appears heavily weathered and may include iron oxides.

Formation & geological history

Likely formed in hydrothermal veins or magmatic sulfide deposits, commonly millions to billions of years old. Surface weathering oxidizes sulfides to reddish-brown iron oxides and copper-bearing minerals.

Uses & applications

Chalcopyrite is an important copper ore; attractive crystals are collected, but this rough fragment has little jewelry or construction use.

Geological facts

Chalcopyrite is commonly mistaken for gold, but it is softer, less dense, and often shows iridescent tarnish. A streak test, hardness test, and copper assay are more reliable than color alone.

Field identification & locations

Look for brassy metallic color, green-black or brown oxidation, and a dark streak; it should not scratch glass. Common localities include porphyry-copper and volcanogenic massive-sulfide districts worldwide.