![Turquoise (Hydrated phosphate of copper and aluminium [CuAl6(PO4)4(OH)8·4H2O]) — mineral](https://media.rockidentification.com/e0686657-6bf2-47dd-93e5-405c9ea60c49-compressed.jpg)
mineral
Turquoise
Hydrated phosphate of copper and aluminium [CuAl6(PO4)4(OH)8·4H2O]
Hardness: 5.0–6.0 (Mohs); Color: Sky-blue to greenish-blue; Luster: Waxy to sub-vitreous; Crystal Structure: Triclinic; Cleavage: Perfect; Specific Gravity: 2.6–2.9
- Hardness
- 5
- Color
- Sky-blue to greenish-blue
- Luster
- Waxy to sub-vitreous
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Physical properties
Hardness: 5.0–6.0 (Mohs); Color: Sky-blue to greenish-blue; Luster: Waxy to sub-vitreous; Crystal Structure: Triclinic; Cleavage: Perfect; Specific Gravity: 2.6–2.9
Formation & geological history
Formed through the infiltration of meteoric acidic solutions during the weathering and oxidation of pre-existing minerals. It is a secondary mineral usually found in volcanic rocks or arid environments.
Uses & applications
Predominantly used as a gemstone in jewelry (cabochons, beads, and inlay) and for ornamental decorative objects. Highly valued in traditional Southwestern and Middle Eastern artistry.
Geological facts
Persians called it 'píruzeh' (victory) and the name Turquoise comes from the French 'turquois' (Turkish), as it was originally brought to Europe from Iranian mines through Turkey.
Field identification & locations
Identify by its waxy luster, sky-blue 'Robin's Egg' color, and lack of transparency. Common locations include Iran, Arizona (USA), Nevada (USA), and China.
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mineral