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); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal Structure: Triclinic (usually massive); Cleavage: Perfect but rarely seen.

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

Hardness: 5-6 (Mohs); Color: Sky blue to blue-green; Luster: Waxy to subvitreous; Crystal Structure: Triclinic (usually massive); Cleavage: Perfect but rarely seen.

Formation & geological history

Secondary mineral formed in the oxidation zone of copper deposits. It is deposited by circulating waters in arid environments within volcanic and sedimentary rocks.

Uses & applications

Primarily used in jewelry (cabochons, beads, and inlay) and as an ornamental stone in many cultures.

Geological facts

One of the oldest known gemstones, it was heavily mined by the Ancient Egyptians since 3000 BC. In Navajo culture, it represents health and protection.

Field identification & locations

Look for copper-rich host rocks in arid regions like Arizona, Iran, or China. Can be identified by its color and solubility in hydrochloric acid (test with caution).