
mineral
Native Copper
Copper (Cu)
Mohs hardness: 2.5 to 3; Color: distinctive copper-red, often tarnishing to brown or green; Luster: metallic; Crystal structure: isometric; Cleavage: none, exhibits hackly fracture; Specific gravity: 8.9
- Hardness
- 2
- Color
- distinctive copper-red, often tarnishing to brown or green
- Luster
- metallic
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Physical properties
Mohs hardness: 2.5 to 3; Color: distinctive copper-red, often tarnishing to brown or green; Luster: metallic; Crystal structure: isometric; Cleavage: none, exhibits hackly fracture; Specific gravity: 8.9
Formation & geological history
Formed as a precipitate in hydrothermal veins, in cavities of basaltic lavas, and through the oxidation of copper sulfide deposits
Uses & applications
Extensively used for electrical wiring, plumbing, coinage, industrial machinery, and sought after by mineral collectors
Geological facts
Native copper is one of the few metallic elements to occur in native form in large quantities, with the Keweenaw Peninsula in Michigan historically famous for massive native copper deposits
Field identification & locations
Easily identified by its characteristic reddish-brown metallic luster, high density (heavy for its size), malleability, and green tarnish (patina); commonly found in major copper-producing regions worldwide
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