
mineral
Turquoise
Hydrated copper aluminum phosphate, CuAl6(PO4)4(OH)8·4H2O
AI-generated identification · may be incorrectHardness: 5 to 6 on the Mohs scale. Color: Blue, bluish-green, green. Luster: Waxy to subvitreous. Crystal Structure: Triclinic. Cleavage: Perfect in one direction, good in another, but rarely seen. Specific Gravity: 2.60 to 2.90.
- Hardness
- 5 to 6 on the Mohs scale
- Color
- Blue, bluish-green, green
- Luster
- Waxy to subvitreous
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Physical properties
Hardness: 5 to 6 on the Mohs scale. Color: Blue, bluish-green, green. Luster: Waxy to subvitreous. Crystal Structure: Triclinic. Cleavage: Perfect in one direction, good in another, but rarely seen. Specific Gravity: 2.60 to 2.90.
Formation & geological history
Forms in arid regions through the weathering and oxidation of pre-existing copper-bearing minerals, typically in weathered volcanic or sedimentary rocks where descending water percolates through copper-rich aluminum rocks.
Uses & applications
Widely used in jewelry, ornamental carvings, inlay work, and as a collector's gemstone.
Geological facts
Turquoise is one of the world's most ancient gem materials, prized by the ancient Egyptians, Persians, and Native Americans for thousands of years as a talisman of protection and good fortune.
Field identification & locations
Easily identified by its distinct robin's-egg blue or greenish-blue color often interspersed with dark brown or black web-like matrix veins. Found in regions such as the southwestern United States, Iran, China, and Sinai.
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