Rock Identifier
Turquoise-bead jewelry (Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O; the beads may be natural turquoise or a stabilized/imitation material) — gemstone
gemstone

Turquoise-bead jewelry

Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O; the beads may be natural turquoise or a stabilized/imitation material

AI-generated identification · may be incorrect

Opaque blue beads with dark veining and a polished luster; turquoise is triclinic, typically Mohs 5–6, and has a specific gravity of about 2.6–2.9. The photo does not establish whether these beads are natural, treated, or imitation.

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Physical properties

Opaque blue beads with dark veining and a polished luster; turquoise is triclinic, typically Mohs 5–6, and has a specific gravity of about 2.6–2.9. The photo does not establish whether these beads are natural, treated, or imitation.

Formation & geological history

Natural turquoise forms as a secondary copper-aluminum phosphate in weathered, arid-zone deposits; geological ages vary by deposit. The pictured jewelry is assembled and may include treated beads.

Uses & applications

Used for beads, cabochons, and ornamental jewelry; turquoise is also collected as a mineral specimen.

Geological facts

Turquoise color ranges from sky blue to green, and dark matrix may preserve traces of its host rock. Howlite and dyed materials are common turquoise simulants.

Field identification & locations

The image shows polished blue-green beads, but appearance alone cannot confirm turquoise; check for natural matrix and seek gemological testing for identification and treatment. Major sources include Iran, the southwestern United States, China, and Egypt.