Rock Identifier
Polished turquoise cabochon pendant (Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O) — mineral
mineral

Polished turquoise cabochon pendant

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

AI-generated identification · may be incorrect

Opaque blue-green, waxy to subvitreous luster, commonly brown or black limonite matrix; Mohs hardness 5–6, triclinic structure, no prominent cleavage, specific gravity about 2.6–2.9. The pictured stone is polished and mounted in metal.

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Physical properties

Opaque blue-green, waxy to subvitreous luster, commonly brown or black limonite matrix; Mohs hardness 5–6, triclinic structure, no prominent cleavage, specific gravity about 2.6–2.9. The pictured stone is polished and mounted in metal.

Formation & geological history

Forms as a secondary mineral in arid, copper-rich, phosphate-bearing rocks through groundwater alteration, commonly during Cenozoic weathering. Major deposits occur in Iran, the southwestern United States, China, Chile, and Mexico.

Uses & applications

Used for cabochons, beads, inlay, carvings, and ornamental jewelry; historically valued as a decorative and symbolic stone. It has little industrial use.

Geological facts

Color ranges from sky blue to green depending largely on copper, iron, and zinc content; matrix patterns can help indicate locality. Much commercial turquoise is stabilized with resin, reconstituted, dyed, or simulated.

Field identification & locations

Identify by its opaque blue-green color, relatively soft feel, waxy polish, and natural matrix; glassy translucence or extreme hardness suggests an imitation. Common localities include Arizona, Nevada, New Mexico, Iran, and Hubei, China.