Rock Identifier
Blue-green cabochon pendant, likely turquoise or composite turquoise (Turquoise: hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O; exact identification is uncertain from the blurred image) — gemstone
gemstone

Blue-green cabochon pendant, likely turquoise or composite turquoise

Turquoise: hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O; exact identification is uncertain from the blurred image

AI-generated identification · may be incorrect

The visible inset appears opaque blue-green with possible dark matrix, set in metal jewelry. Turquoise has Mohs hardness 5–6, waxy to subvitreous luster, cryptocrystalline structure, and no obvious cleavage.

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Physical properties

The visible inset appears opaque blue-green with possible dark matrix, set in metal jewelry. Turquoise has Mohs hardness 5–6, waxy to subvitreous luster, cryptocrystalline structure, and no obvious cleavage.

Formation & geological history

Turquoise forms as a secondary mineral in arid, copper-rich environments through groundwater alteration, commonly in Cenozoic to older host rocks. Jewelry may also use stabilized, reconstructed, or dyed turquoise.

Uses & applications

Used primarily in jewelry and ornamental carving; high-quality natural turquoise is collectible, while stabilized or composite material is more common and less valuable.

Geological facts

Color ranges from sky blue to green depending on copper, iron, and zinc content. The blurred specimen could alternatively be dyed howlite, glass, or another blue-green stone.

Field identification & locations

Check for natural irregular matrix, an opaque body, moderate softness, and a cool stone feel; avoid scratch or chemical tests on jewelry. Major sources include Arizona, Nevada, Iran, China, and Mexico.