Rock Identifier
Polished turquoise-matrix cabochon (Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O, with iron-rich matrix and possible chrysocolla) — mineral
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 incorrect

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.

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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.