Rock Identifier
Turquoise beads (Turquoise, a hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O; some beads may be dyed or stabilized howlite or magnesite.) — gemstone
gemstone

Turquoise beads

Turquoise, a hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O; some beads may be dyed or stabilized howlite or magnesite.

AI-generated identification · may be incorrect

Opaque vivid blue to blue-green, typically waxy to subvitreous and Mohs 5–6; triclinic, with no prominent cleavage. The beads’ uniform color and visible matrix are not enough to confirm natural turquoise or treatment from the image alone.

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Physical properties

Opaque vivid blue to blue-green, typically waxy to subvitreous and Mohs 5–6; triclinic, with no prominent cleavage. The beads’ uniform color and visible matrix are not enough to confirm natural turquoise or treatment from the image alone.

Formation & geological history

Turquoise forms as a secondary mineral in arid-zone oxidation of copper deposits, often replacing host rock; deposits range in age and occur in Iran, the southwestern United States, China, and elsewhere.

Uses & applications

Cut and polished for jewelry and ornament; lower-grade material is used for beads, inlay, and craftwork.

Geological facts

Its color comes chiefly from copper, while iron can shift it toward green. Stabilization with resin is common in commercial turquoise jewelry.

Field identification & locations

The image shows polished blue beads, but a gemological test is needed to distinguish turquoise from dyed imitations and identify treatments. Natural turquoise often has irregular color and matrix; value depends on authenticity, quality, origin, and workmanship.