Rock Identifier
Turquoise (Turquoise (Hydrated phosphate of copper and aluminium), CuAl6(PO4)4(OH)84H2O) — mineral
mineral

Turquoise

Turquoise (Hydrated phosphate of copper and aluminium), CuAl6(PO4)4(OH)84H2O

Hardness: 5–6; Color: Sky-blue to green-blue; Luster: Waxy to subvitreous; Crystal system: Triclinic; Cleavage: Perfect (rarely seen in massive forms); Specific Gravity: 2.6–2.9

Hardness
5–6
Color
Sky-blue to green-blue
Luster
Waxy to subvitreous
Identified More mineral
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Physical properties

Hardness: 5–6; Color: Sky-blue to green-blue; Luster: Waxy to subvitreous; Crystal system: Triclinic; Cleavage: Perfect (rarely seen in massive forms); Specific Gravity: 2.6–2.9

Formation & geological history

A secondary mineral formed by the percolation of acidic aqueous solutions during the weathering and oxidation of pre-existing minerals. Typically found in arid regions within volcanic rocks or sedimentary environments.

Uses & applications

Primarily used as a gemstone in jewelry (cabochons, beads, inlays) and for ornamental carvings. Historically significant in Native American and Persian cultures.

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 'turquois', meaning 'Turkish', as it first reached Europe via Turkey.

Field identification & locations

Identify in the field by its distinct robin's egg blue color and waxy appearance. Often found in veinlets or nodules. Collectors should look for 'Sleeping Beauty' or 'Kingman' varieties in the Southwestern USA.