
mineral
Polished turquoise-matrix cabochon
Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O, with iron-rich matrix and possible chrysocolla
AI-generated identification · may be incorrectBlue-green to dark green, mottled with brown/gray host matrix; waxy to subvitreous luster and opaque, microcrystalline structure. Mohs hardness 5–6; specific gravity about 2.6–2.9; no prominent cleavage.
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Physical properties
Blue-green to dark green, mottled with brown/gray host matrix; waxy to subvitreous luster and opaque, microcrystalline structure. Mohs hardness 5–6; specific gravity about 2.6–2.9; no prominent cleavage.
Formation & geological history
Forms as a secondary phosphate mineral in arid, oxidized copper deposits, commonly replacing or filling fractures in volcanic or sedimentary host rocks. Most deposits are Cenozoic to older hydrothermal-weathering systems; the exact age is locality-dependent.
Uses & applications
Used for cabochons, beads, carvings, and ornamental objects; historically important in jewelry and ceremonial art. Matrix-rich material is generally less valuable than clear, evenly colored turquoise.
Geological facts
The blue-green color comes mainly from copper, while iron commonly shifts it toward green and produces brown webbing or matrix. Polishing can enhance contrast but may involve stabilization with resin.
Field identification & locations
Identify by its opaque blue-green color, relatively low hardness, waxy luster, and copper-stained matrix; avoid confusing it with dyed howlite, magnesite, or plastic. Common sources include Iran, Arizona, Nevada, China, Mexico, and Chile.
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