Rock Identifier
Turquoise ring stone (likely stabilized or dyed turquoise) (Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O) — gemstone
gemstone

Turquoise ring stone (likely stabilized or dyed turquoise)

Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O

AI-generated identification · may be incorrect

Blue to blue-green, typically opaque with a waxy to subvitreous luster; Mohs hardness 5–6, cryptocrystalline structure, no prominent cleavage, and specific gravity about 2.6–2.9. The photograph shows a polished cabochon set in metal, with possible matrix or treatment.

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Physical properties

Blue to blue-green, typically opaque with a waxy to subvitreous luster; Mohs hardness 5–6, cryptocrystalline structure, no prominent cleavage, and specific gravity about 2.6–2.9. The photograph shows a polished cabochon set in metal, with possible matrix or treatment.

Formation & geological history

Forms as a secondary mineral in arid, copper-rich zones through weathering and groundwater alteration of aluminum-bearing rocks. Important deposits occur in Iran, the southwestern United States, China, Egypt, and Chile; its geological age varies by deposit.

Uses & applications

Used primarily in rings, beads, carvings, and ornamental objects; historically valued as a talisman and decorative gemstone. Stabilization with resin is common for jewelry durability, while dyed imitations also occur.

Geological facts

Turquoise is among the earliest gemstones used by humans. Its color can darken or change with porosity, oils, heat, and chemicals.

Field identification & locations

Identify it by its opaque blue-green color, relatively soft surface, and nonmetallic luster; genuine material may show brown or black limonite matrix. Exact identification requires testing or examination outside the setting, since dyed howlite, magnesite, and composite stones can look similar.