![Malachite (Copper(II) carbonate hydroxide [Cu2CO3(OH)2]) — mineral](https://media.rockidentification.com/5bcf6ff9-fe1f-4471-8615-6d286a80f104-compressed.jpg)
mineral
Malachite
Copper(II) carbonate hydroxide [Cu2CO3(OH)2]
Hardness: 3.5-4.0; Color: Bright green to dark green with distinctive banding; Luster: Adamantine to vitreous or silky; Crystal system: Monoclinic; Cleavage: Perfect; Specific Gravity: 3.6-4.0.
- Hardness
- 3
- Color
- Bright green to dark green with distinctive banding
- Luster
- Adamantine to vitreous or silky
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Physical properties
Hardness: 3.5-4.0; Color: Bright green to dark green with distinctive banding; Luster: Adamantine to vitreous or silky; Crystal system: Monoclinic; Cleavage: Perfect; Specific Gravity: 3.6-4.0.
Formation & geological history
Formed in the oxidized zones of copper deposits where copper-bearing solutions react with carbonate rocks. It is a secondary mineral often found associated with azurite, goethite, and calcite.
Uses & applications
Used primarily as an ornamental stone, in jewelry (cabochons and beads), and historically as a green pigment for paints throughout antiquity. It is also an ore of copper.
Geological facts
Malachite is famous for its 'eyes' or concentric banding. In ancient Egypt, it was ground into powder and used as eye shadow. It is often found intergrown with blue azurite, creating a stunning mineral called 'Azurmalachite'.
Field identification & locations
Identify by its distinctive green banding and light green streak. In the field, it reacts (effervesces) with cold dilute hydrochloric acid. Common locations include the Democratic Republic of the Congo, Russia (Ural Mountains), and Arizona, USA.
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