Rock Identifier
Turquoise-colored stone bead necklace (Likely turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O), but the bead may be dyed or another blue-green stone) — gemstone
gemstone

Turquoise-colored stone bead necklace

Likely turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O), but the bead may be dyed or another blue-green stone

AI-generated identification · may be incorrect

The rounded bead is polished, blue-green with dark matrix-like mottling; turquoise has Mohs hardness 5–6, a waxy to dull luster, and a triclinic crystal structure. The image alone cannot confirm the bead’s material; the pendant appears to be a metal Chinese cash coin, not a geological specimen.

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Physical properties

The rounded bead is polished, blue-green with dark matrix-like mottling; turquoise has Mohs hardness 5–6, a waxy to dull luster, and a triclinic crystal structure. The image alone cannot confirm the bead’s material; the pendant appears to be a metal Chinese cash coin, not a geological specimen.

Formation & geological history

Natural turquoise forms through near-surface alteration of copper-bearing rocks in arid environments; deposits range from geologically recent to hundreds of millions of years old. The bead has been shaped and polished.

Uses & applications

Turquoise is used in jewelry and ornamental objects; this piece is a necklace pendant.

Geological facts

Turquoise’s color comes chiefly from copper, while iron can contribute greener tones. Matrix patterns are host-rock remnants or, in imitations, may be artificially added.

Field identification & locations

Turquoise commonly occurs in Iran, the southwestern United States, China, and other arid regions. Confirm identity with gemological testing rather than relying on color alone.