
mineral
Turquoise (set in silver jewelry)
Turquoise - CuAl6(PO4)4(OH)8·4H2O (Hydrated copper and aluminum phosphate)
AI-generated identification · may be incorrectHardness: 5-6 (Mohs scale), Color: Sky blue to apple green, Luster: Waxy to subvitreous, Crystal Structure: Triclinic (usually cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
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Physical properties
Hardness: 5-6 (Mohs scale), Color: Sky blue to apple green, Luster: Waxy to subvitreous, Crystal Structure: Triclinic (usually cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
Formation & geological history
Formed by the percolation of acidic aqueous solutions during the weathering and oxidation of pre-existing minerals. It is a secondary mineral usually found in arid regions within volcanic or sedimentary host rocks.
Uses & applications
Primarily used in jewelry (cabochons, beads, and inlay) and ornamental carvings. It has been a prized gemstone for over 3,000 years.
Geological facts
Turquoise was one of the first gemstones ever mined; the ancient Egyptians mined it in the Sinai Peninsula as far back as 3000 BCE. Its name comes from the French 'turquois' meaning 'Turkish', as it first reached Europe via Turkey.
Field identification & locations
Identify by its unique blue-green color and 'matrix' (web-like veins of host rock). Often found in copper-rich deposits in the Southwestern USA, China, and Iran. Collectors should check for stabilization treatments or dye.
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