
mineral
Polished turquoise cabochon jewelry (likely composite or stabilized turquoise)
Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O
AI-generated identification · may be incorrectBlue-green opaque cabochons with mottled brown/black matrix, waxy to subvitreous luster, cryptocrystalline structure, no visible cleavage, Mohs hardness about 5–6, and specific gravity around 2.6–2.9. The central oval appears mounted in silver-colored metal; adjacent pieces may include other gemstones.
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Physical properties
Blue-green opaque cabochons with mottled brown/black matrix, waxy to subvitreous luster, cryptocrystalline structure, no visible cleavage, Mohs hardness about 5–6, and specific gravity around 2.6–2.9. The central oval appears mounted in silver-colored metal; adjacent pieces may include other gemstones.
Formation & geological history
Turquoise forms as a secondary phosphate mineral in arid, copper-rich, aluminum-bearing rocks, commonly replacing host rock in shallow veins and cavities. Deposits are generally geologically young relative to their host rocks, often associated with weathering and groundwater circulation.
Uses & applications
Used extensively in cabochon jewelry, carvings, beads, and collectibles; lower-grade material is often stabilized with resin or reconstructed from fragments. Quality depends on color, matrix pattern, natural status, origin, and workmanship.
Geological facts
Persian, American Southwestern, Egyptian, and Chinese turquoise are historically important. Bright, even sky-blue color is generally more valuable than heavily matrixed or green material, although attractive matrix can be desirable.
Field identification & locations
Identify by its opaque blue-green color, relatively low hardness, and waxy surface; beware dyed howlite, plastic, and glass imitations. Common sources include Arizona, Nevada, New Mexico, Iran, China, and Mexico.
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