
mineral
Turquoise cabochon pendant
Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O; likely stabilized or imitation turquoise
AI-generated identification · may be incorrectBlue-green opaque, waxy to subvitreous luster, irregular dark matrix veining, typically cryptocrystalline and massive; Mohs hardness 5–6, specific gravity about 2.6–2.9, no visible cleavage. The smooth teardrop is a polished cabochon set in jewelry.
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Physical properties
Blue-green opaque, waxy to subvitreous luster, irregular dark matrix veining, typically cryptocrystalline and massive; Mohs hardness 5–6, specific gravity about 2.6–2.9, no visible cleavage. The smooth teardrop is a polished cabochon set in jewelry.
Formation & geological history
Turquoise forms as a secondary mineral in arid, oxidized copper deposits, commonly replacing aluminum-rich rock; deposits are generally Cenozoic to older hydrothermal-weathering systems. The pendant has been cut, polished, drilled, and mounted with a metal bail.
Uses & applications
Used primarily for cabochons, beads, inlay, and ornamental jewelry; historically important in Persian, Egyptian, and Native American art. Fine natural material is collectible, while stabilized or reconstructed material is less valuable.
Geological facts
The web-like brown matrix may be limonite or host rock, but uniform color and extensive veining can also indicate dyed magnesite or reconstituted turquoise. Turquoise is the birthstone for December.
Field identification & locations
Common sources include Iran, the southwestern United States, China, Chile, and Mexico. Natural turquoise feels slightly cool, is opaque, and scratches glass only poorly; acetone or heat tests can damage treatments, so laboratory testing is preferable.
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