
mineral
Turquoise
Turquoise (Hydrated phosphate of copper and aluminium), CuAl6(PO4)4(OH)8·4H2O
Hardness: 5–6 (Mohs); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal system: Triclinic; Specific Gravity: 2.6–2.9; Cleavage: Good to perfect (though rarely seen in massive specimens)
- Hardness
- 5–6 (Mohs)
- Color
- Sky blue to blue-green
- Luster
- Waxy to subvitreous
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Physical properties
Hardness: 5–6 (Mohs); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal system: Triclinic; Specific Gravity: 2.6–2.9; Cleavage: Good to perfect (though rarely seen in massive specimens)
Formation & geological history
A secondary mineral formed by the percolation of acidic aqueous solutions during the weathering and oxidation of pre-existing copper-bearing minerals. Typically found in arid regions within volcanic rocks or sedimentary phosphate-rich layers.
Uses & applications
Primarily used in jewelry, decorative carvings, and as a gemstone for collectors. Historically used in amulets and architectural inlay.
Geological facts
Turquoise is one of the oldest known gemstones, used by the Egyptians as early as 3000 BCE. Its name comes from the French 'turqueise', meaning 'Turkish', as it first reached Europe via Turkey from Persian mines.
Field identification & locations
Identified by its unique 'robin's egg' blue color and often presence of a dark matrix (veins of host rock). It is commonly found in the Southwestern USA, Iran, and China. Collectors should look for vibrancy of color and lack of artificial stabilization.
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