Rock Identifier
Turquoise cabochon ring (Turquoise, hydrated copper aluminum phosphate (CuAl₆(PO₄)₄(OH)₈·4H₂O); the stones may be stabilized or treated) — gemstone
gemstone

Turquoise cabochon ring

Turquoise, hydrated copper aluminum phosphate (CuAl₆(PO₄)₄(OH)₈·4H₂O); the stones may be stabilized or treated

AI-generated identification · may be incorrect

Opaque blue-green stones with a waxy-to-subvitreous polish, set as cabochons; Mohs hardness 5–6, triclinic crystal system, typically no visible cleavage. The image alone cannot confirm whether the stones are natural turquoise or identify any treatment; the surrounding setting appears to be metal.

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Physical properties

Opaque blue-green stones with a waxy-to-subvitreous polish, set as cabochons; Mohs hardness 5–6, triclinic crystal system, typically no visible cleavage. The image alone cannot confirm whether the stones are natural turquoise or identify any treatment; the surrounding setting appears to be metal.

Formation & geological history

Turquoise forms when copper-bearing fluids alter aluminum- and phosphorus-rich rocks, often in arid-zone deposits. Deposits range from ancient to geologically recent; the stones’ specific origin and age cannot be determined from the photograph.

Uses & applications

Used chiefly in jewelry and ornamental objects; historically valued by many cultures. Turquoise is also collected as a mineral specimen.

Geological facts

Its characteristic blue-green color comes largely from copper, with iron often contributing green tones. Natural turquoise is commonly stabilized with resin to improve durability and color.

Field identification & locations

Look for opaque blue-to-green color and, in some stones, a natural matrix pattern; color alone cannot authenticate it. Major sources include the southwestern United States, Iran, China, and Mexico; gemological testing can distinguish turquoise from imitation materials.