Rock Identifier
Turquoise (Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O) — mineral
mineral

Turquoise

Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O

AI-generated identification · may be incorrect

Blue-green, opaque, waxy to subvitreous luster; Mohs hardness 5–6, cryptocrystalline structure, no visible cleavage, and specific gravity about 2.6–2.9. The orange-brown areas may be matrix or iron staining; the piece appears polished or tumbled.

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Physical properties

Blue-green, opaque, waxy to subvitreous luster; Mohs hardness 5–6, cryptocrystalline structure, no visible cleavage, and specific gravity about 2.6–2.9. The orange-brown areas may be matrix or iron staining; the piece appears polished or tumbled.

Formation & geological history

Forms as a secondary phosphate mineral in arid, copper-rich, weathered volcanic or sedimentary rocks, generally by low-temperature groundwater alteration. Most deposits are geologically young compared with their host rocks, commonly Cenozoic.

Uses & applications

Used as a cabochon gemstone, beads, carvings, and decorative objects; historically important in jewelry and ceremonial artifacts. Lower-grade material is also used for inexpensive inlay and polished specimens.

Geological facts

Its color comes mainly from copper, while iron can shift it toward green or brown. Natural turquoise is commonly stabilized with resin, and dyed imitations or reconstructed turquoise are widespread.

Field identification & locations

Identify it by its opaque blue-green color, relatively soft surface, waxy luster, and often brown or black matrix; it should not show glass-like transparency. Common sources include Iran, the southwestern United States, China, Mexico, Chile, and Egypt.