Rock Identifier
Turquoise (Hydrated phosphate of copper and aluminium [CuAl6(PO4)4(OH)8·4H2O]) — mineral
mineral

Turquoise

Hydrated phosphate of copper and aluminium [CuAl6(PO4)4(OH)8·4H2O]

Hardness: 5-6 (Mohs scale); Color: Sky blue to apple green; Luster: Waxy to subvitreous; Crystal Structure: Triclinic (rarely found in crystal form, usually cryptocrystalline masses); Cleavage: Perfect (rarely seen); Specific Gravity: 2.6-2.9.

Hardness
5-6 (Mohs scale)
Color
Sky blue to apple green
Luster
Waxy to subvitreous
Identified More mineral

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Physical properties

Hardness: 5-6 (Mohs scale); Color: Sky blue to apple green; Luster: Waxy to subvitreous; Crystal Structure: Triclinic (rarely found in crystal form, usually cryptocrystalline masses); Cleavage: Perfect (rarely seen); Specific Gravity: 2.6-2.9.

Formation & geological history

Formed as a secondary mineral by the action of percolating acidic solutions during the weathering and oxidation of pre-existing minerals (copper-bearing rocks) in arid climates. It often fills veins or occurs as crusts in volcanic rocks.

Uses & applications

Primarily used as a gemstone and ornamental stone in jewelry, carvings, and inlays. Especially significant in Native American, Persian, and Egyptian cultural artistry.

Geological facts

It is one of the oldest gemstones in human history, used by Egyptians as far back as 3000 BCE. The name comes from the French word 'turquois', meaning 'Turkish', as the stone first reached Europe through Turkish trade routes.

Field identification & locations

Identify by its unique 'robin's egg' blue color and dark spider-web-like veins (matrix) made of limonite or manganese oxide. Commonly found in the Southwestern USA (Arizona, Nevada), Iran, and China. In the field, look for sky-blue outcrops in weathered igneous rocks near copper deposits.