Rock Identifier
Blue-green copper mineral-bearing rock, likely chrysocolla with malachite (Chrysocolla (hydrated copper aluminosilicate, approximately (Cu,Al)₂H₂Si₂O₅(OH)₄·nH₂O) with malachite (Cu₂CO₃(OH)₂), possibly in altered host rock) — mineral
mineral

Blue-green copper mineral-bearing rock, likely chrysocolla with malachite

Chrysocolla (hydrated copper aluminosilicate, approximately (Cu,Al)₂H₂Si₂O₅(OH)₄·nH₂O) with malachite (Cu₂CO₃(OH)₂), possibly in altered host rock

AI-generated identification · may be incorrect

Typically turquoise-blue to green, opaque, earthy to waxy or vitreous luster, amorphous or cryptocrystalline, and Mohs hardness about 2.5–4; malachite commonly forms green bands or patches. The specimens appear rough and massive, with no obvious cleavage.

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Physical properties

Typically turquoise-blue to green, opaque, earthy to waxy or vitreous luster, amorphous or cryptocrystalline, and Mohs hardness about 2.5–4; malachite commonly forms green bands or patches. The specimens appear rough and massive, with no obvious cleavage.

Formation & geological history

Forms in oxidized zones above copper deposits when copper-rich fluids alter silica- and aluminum-bearing rock; commonly associated with quartz, limonite, azurite, and native copper. Formation is generally geologically young relative to the host deposit, occurring during near-surface weathering.

Uses & applications

Used as a decorative stone, cabochon material, pigment historically, and copper ore when abundant; attractive polished material has modest lapidary value.

Geological facts

Chrysocolla’s intense blue-green color comes from hydrated copper; it is often sold commercially as “chrysocolla-malachite” or “gem silica” when silica-rich and durable.

Field identification & locations

Look for blue-green color, irregular mottling, association with brown iron oxides, and a soft scratch response; avoid acids and prolonged soaking. Common localities include Arizona, Nevada, Chile, Peru, the Democratic Republic of Congo, and Russia.