Rock Identifier
Tumbled turquoise-bearing stone (likely turquoise or chrysocolla) (Turquoise: CuAl₆(PO₄)₄(OH)₈·4H₂O; possible chrysocolla: hydrated copper silicate) — mineral
mineral

Tumbled turquoise-bearing stone (likely turquoise or chrysocolla)

Turquoise: CuAl₆(PO₄)₄(OH)₈·4H₂O; possible chrysocolla: hydrated copper silicate

AI-generated identification · may be incorrect

Small polished/tumbled specimen with blue-green color and gray-brown matrix; typically waxy to dull luster, cryptocrystalline structure, no visible cleavage, and Mohs hardness about 2–6 (turquoise ~5–6; chrysocolla ~2–4).

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Physical properties

Small polished/tumbled specimen with blue-green color and gray-brown matrix; typically waxy to dull luster, cryptocrystalline structure, no visible cleavage, and Mohs hardness about 2–6 (turquoise ~5–6; chrysocolla ~2–4).

Formation & geological history

Copper-rich groundwater alters aluminum- or silica-bearing rocks, forming turquoise or chrysocolla in veins and cavities, generally in arid regions over geologically recent to ancient weathering zones.

Uses & applications

Used as a semiprecious gemstone, beads, carvings, and decorative objects; softer material is often stabilized, dyed, or coated for durability.

Geological facts

Blue-green copper minerals can be difficult to distinguish visually, and many commercial specimens are composites or treated. A matrix pattern is common in turquoise from several deposits.

Field identification & locations

Common sources include Iran, the American Southwest, Mexico, Chile, China, and Australia. Confirm identity with hardness, specific gravity, magnification, and professional testing; avoid destructive tests on polished pieces.