
mineral
Copper-bearing rock (likely native copper in a green copper-mineral matrix)
Native copper (Cu), possibly with chrysocolla or malachite; exact identification requires testing
AI-generated identification · may be incorrectGreen-blue, matte to earthy matrix with irregular salmon-red metallic-looking veins or patches. Native copper has Mohs hardness 2.5–3 and metallic luster; the image alone does not establish crystal structure or specific gravity.
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Physical properties
Green-blue, matte to earthy matrix with irregular salmon-red metallic-looking veins or patches. Native copper has Mohs hardness 2.5–3 and metallic luster; the image alone does not establish crystal structure or specific gravity.
Formation & geological history
Likely formed when copper-rich fluids deposited copper and secondary copper minerals in fractures during oxidation of a copper deposit; age depends on locality and cannot be determined from the image.
Uses & applications
Copper ores are mined for electrical wiring, plumbing, alloys, and other industrial uses; attractive specimens may be collected or used decoratively.
Geological facts
Copper commonly develops green-blue secondary minerals as it weathers, while unoxidized native copper can retain a reddish metallic color.
Field identification & locations
Look for metallic reddish areas that are malleable and leave a copper-colored streak, alongside blue-green staining. Copper-bearing specimens occur in many mining districts, notably Michigan’s Keweenaw Peninsula; this image does not confirm a locality or species.
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