
mineral
Polished copper-bearing rock, likely cuprite-rich copper ore
Cuprite (Cu₂O) with native copper and iron-oxide matrix, probable
AI-generated identification · may be incorrectRusty red-brown, earthy to submetallic luster, rounded/tumbled surface with darker pits and inclusions. Cuprite has Mohs hardness 3.5–4, cubic crystals, no prominent cleavage, and high specific gravity (~6.0); exact properties vary with matrix.
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Physical properties
Rusty red-brown, earthy to submetallic luster, rounded/tumbled surface with darker pits and inclusions. Cuprite has Mohs hardness 3.5–4, cubic crystals, no prominent cleavage, and high specific gravity (~6.0); exact properties vary with matrix.
Formation & geological history
Forms in the oxidized zone of copper deposits when primary copper sulfides weather, commonly alongside native copper, malachite, azurite, and limonite. Such ores are generally geologically young relative to their host deposits, often Cenozoic to Precambrian depending on locality.
Uses & applications
Primarily a collector specimen; copper ores may historically be mined for copper, but this small polished piece has no practical industrial use. Attractive red material can be used decoratively or in mineral displays.
Geological facts
The vivid red color is characteristic of cuprite, though the specimen may also contain reddish iron oxides or jasper. Cuprite can darken or develop green copper-carbonate coatings with prolonged weathering.
Field identification & locations
Commonly found in oxidized copper districts such as Arizona, Namibia, Chile, Russia, and Australia. Confirm with a streak test (cuprite gives reddish-brown streak), unusually high heft, and—where safe—hardness testing; visual identification alone is uncertain.
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