Rock Identifier
Turquoise bead necklace (Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O; likely stabilized or imitation beads cannot be ruled out from the image) — gemstone
gemstone

Turquoise bead necklace

Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O; likely stabilized or imitation beads cannot be ruled out from the image

AI-generated identification · may be incorrect

Opaque blue-green beads with dark matrix-like veining and polished surfaces; turquoise is Mohs 5–6, waxy to subvitreous, and triclinic. Necklace findings and possible treatments are not geological material.

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Physical properties

Opaque blue-green beads with dark matrix-like veining and polished surfaces; turquoise is Mohs 5–6, waxy to subvitreous, and triclinic. Necklace findings and possible treatments are not geological material.

Formation & geological history

Natural turquoise forms in arid-zone copper deposits as a secondary phosphate mineral, commonly by groundwater alteration of copper-bearing rocks. Deposits range from geologically young to ancient; the pictured beads’ source and age are unknown.

Uses & applications

Used in jewelry and decorative objects; gold-colored spacers are non-geological components.

Geological facts

Turquoise’s color comes chiefly from copper, while iron can shift it toward green. Beads are often stabilized with resin to improve durability and color consistency.

Field identification & locations

Typical turquoise is opaque and blue to green, sometimes with a dark host-rock matrix; appearance alone cannot confirm natural material or treatment. Major sources include Iran, the southwestern United States, China, and Mexico.