
mineral
Turquoise in Matrix
CuAl6(PO4)4(OH)8·4H2O (Hydrated copper aluminum phosphate)
AI-generated identification · may be incorrectHardness: 5-6 on Mohs scale; Color: Sky-blue to bluish-green or apple-green with dark matrix veins; Luster: Waxy to sub-vitreous; Crystal system: Triclinic (usually microcrystalline mass); Specific gravity: 2.6-2.9
- Hardness
- 5-6 on Mohs scale
- Luster
- Waxy to sub-vitreous
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Physical properties
Hardness: 5-6 on Mohs scale; Color: Sky-blue to bluish-green or apple-green with dark matrix veins; Luster: Waxy to sub-vitreous; Crystal system: Triclinic (usually microcrystalline mass); Specific gravity: 2.6-2.9
Formation & geological history
Secondary mineral formed by the percolation of acidic aqueous solutions through copper-bearing and aluminum-rich rocks during the weathering process. Often found in arid or semi-arid hydrothermal copper deposits.
Uses & applications
Widely used as an ornamental gemstone, in traditional Native American and Southwestern jewelry, cabochons, beads, and carved sculptures.
Geological facts
Turquoise is one of the oldest known gemstones, mined since at least 3000 BCE in Sinai. The name originates from the French 'turquois', meaning 'Turkish', as it was brought to Europe via trade routes through Turkey.
Field identification & locations
Identified by its signature robin's egg blue to turquoise-green color with dark brown, black, or metallic host rock matrix veins. Major sources include the US Southwest (Arizona, Nevada), Iran, China, and Mexico.
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