
mineral
Malachite
Copper Carbonate Hydroxide, Cu2CO3(OH)2
AI-generated identification · may be incorrectHardness: 3.5 to 4 on the Mohs scale. Color: Bright green, pale green to dark green. Luster: Adamantine, vitreous, greasy, or dull. Crystal Structure: Monoclinic, typically forming botryoidal, fibrous, or stalactitic masses. Cleavage: Perfect in one direction, good in another, but rarely seen.…
- Hardness
- 3
- Color
- Bright green, pale green to dark green
- Luster
- Adamantine, vitreous, greasy, or dull
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Physical properties
Hardness: 3.5 to 4 on the Mohs scale. Color: Bright green, pale green to dark green. Luster: Adamantine, vitreous, greasy, or dull. Crystal Structure: Monoclinic, typically forming botryoidal, fibrous, or stalactitic masses. Cleavage: Perfect in one direction, good in another, but rarely seen. Specific Gravity: 3.6 to 4.0.
Formation & geological history
Forms as a supergene mineral in the oxidation zone of copper ore deposits, frequently associated with azurite, cuprite, and native copper.
Uses & applications
Used extensively as an ornamental stone, for carvings, beads, and cabochons in jewelry, and historically as a green mineral pigment in paint.
Geological facts
Malachite has been mined for over 3,000 years, notably in the Great Orme in Wales and the Timna Valley in Israel. It is often found together with azurite, creating striking blue and green banded patterns.
Field identification & locations
Easily identified by its characteristic bright green color and effervescence when tested with dilute hydrochloric acid due to its carbonate content. Common in major copper-producing regions worldwide, including the Democratic Republic of Congo, Australia, Russia, and the southwestern United States.
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