
mineral
Native Copper
Copper (Cu)
Mohs hardness: 2.5 to 3, Color: Copper-red, reddish-brown, often with a green tarnish (patina), Luster: Metallic, Crystal system: Isometric, Cleavage: None, Specific gravity: 8.9
- Hardness
- 2
Identified More mineral →
Explore Native Copper in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Mohs hardness: 2.5 to 3, Color: Copper-red, reddish-brown, often with a green tarnish (patina), Luster: Metallic, Crystal system: Isometric, Cleavage: None, Specific gravity: 8.9
Formation & geological history
Formed in hydrothermal veins, as secondary deposits in basaltic lava cavities, and through the oxidation of copper sulfide deposits.
Uses & applications
Electrical wiring, plumbing, coinage, industrial machinery, and decorative or collector items.
Geological facts
Native copper was one of the first metals used by humans, marking the beginning of the Chalcolithic (Copper Age) around 5,000 years ago.
Field identification & locations
Easily identified by its distinctive reddish-copper color, high density, and malleability. Found worldwide, with major deposits in Michigan (USA), Chile, and the Ural Mountains.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
sedimentary
Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral