Rock Identifier
Native copper (probable copper-rich mineral specimen) (Copper, Cu; possibly mixed with cuprite, malachite, and iron-oxide alteration minerals) — mineral
mineral

Native copper (probable copper-rich mineral specimen)

Copper, Cu; possibly mixed with cuprite, malachite, and iron-oxide alteration minerals

AI-generated identification · may be incorrect

Irregular metallic reddish-brown/copper-colored mass with dark oxidation and green-blue patches. Native copper has Mohs hardness 2.5–3, metallic luster, cubic crystal structure, no cleavage, and specific gravity about 8.9; the apparent porous texture may reflect corrosion or matrix loss.

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Physical properties

Irregular metallic reddish-brown/copper-colored mass with dark oxidation and green-blue patches. Native copper has Mohs hardness 2.5–3, metallic luster, cubic crystal structure, no cleavage, and specific gravity about 8.9; the apparent porous texture may reflect corrosion or matrix loss.

Formation & geological history

Likely formed by hydrothermal or supergene enrichment in an oxidized copper deposit; surface alteration can produce cuprite and malachite. Exact age cannot be determined visually. The Yemen region near 15.4°N, 44.2°E has volcanic and mineralized terranes, making copper-bearing material plausible.

Uses & applications

Copper is used in electrical wiring, plumbing, alloys, and ornaments; attractive native-copper specimens are collected, though this piece appears heavily weathered.

Geological facts

Copper commonly develops green patina from malachite or related carbonates. A fresh surface should be copper-red and metallic; copper is highly malleable rather than brittle.

Field identification & locations

Field tests: streak is reddish-copper, conductivity is high, and a steel knife may scratch it; it is nonmagnetic. Confirm with hardness, streak, and preferably chemical/XRF testing, since slag or copper-rich industrial metal is possible.