Rock Identifier
Turquoise bead bracelet (Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O (bead material may be stabilized or dyed)) — gemstone
gemstone

Turquoise bead bracelet

Turquoise, hydrated copper–aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O (bead material may be stabilized or dyed)

AI-generated identification · may be incorrect

Opaque blue, polished beads with a waxy-to-subvitreous luster; Mohs hardness 5–6, triclinic crystal system, poor cleavage. The photo alone cannot confirm whether the beads are natural turquoise or treated material.

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Physical properties

Opaque blue, polished beads with a waxy-to-subvitreous luster; Mohs hardness 5–6, triclinic crystal system, poor cleavage. The photo alone cannot confirm whether the beads are natural turquoise or treated material.

Formation & geological history

Turquoise forms as a secondary mineral in arid-zone weathering deposits, typically where copper-bearing rocks interact with phosphate- and aluminum-rich water. Deposits occur in rocks of many ages.

Uses & applications

Used mainly for jewelry and decorative objects; turquoise is also collected as a gemstone.

Geological facts

The gold-colored fittings are likely metal and are not part of the geological specimen. Turquoise color varies with copper and iron content.

Field identification & locations

Natural turquoise is relatively soft and opaque, often with matrix veining; confirm identity and treatment through a reputable gem laboratory or seller. Major sources include Iran, the southwestern United States, China, and Mexico.