
mineral
Turquoise
Hydrated phosphate of copper and aluminium (CuAl6(PO4)4(OH)8·4H2O)
Hardness: 5-6 (Mohs scale); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal system: Triclinic (rarely macro-crystalline); Fracture: Conchoidal; Specific Gravity: 2.6-2.9
- Hardness
- 5-6 (Mohs scale)
- Color
- Sky blue to blue-green
- Luster
- Waxy to subvitreous
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Physical properties
Hardness: 5-6 (Mohs scale); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal system: Triclinic (rarely macro-crystalline); Fracture: Conchoidal; 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 climates within volcanic rocks or phosphorus-rich sedimentary rocks.
Uses & applications
Primarily used in jewelry (beads, cabochons, inlay) and ornamental objects. Highly valued as a gemstone and collector's item in various cultures.
Geological facts
Turquoise is one of the oldest gemstones in human history; it was mined by the Ancient Egyptians as early as 3000 BCE. Its name comes from the French 'turquois' meaning 'Turkish', as the stone first reached Europe via Turkish trade routes.
Field identification & locations
Identify by its unique robin's egg blue or greenish-blue color and waxy luster. In the field, look for 'matrix' (veins of host rock like limonite or sandstone). Common locations include Iran, Southwestern USA, China, and Mexico.
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