Rock Identifier
Dyed or treated turquoise-like tumbled stone (Likely turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O), though blue-green magnesite or howlite imitation is possible) — mineral
mineral

Dyed or treated turquoise-like tumbled stone

Likely turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O), though blue-green magnesite or howlite imitation is possible

AI-generated identification · may be incorrect

Opaque blue-green body with dark brown/black matrix and waxy-to-glassy polish; turquoise hardness is Mohs 5–6, typically cryptocrystalline and non-cleavable, with specific gravity about 2.6–2.8.

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Physical properties

Opaque blue-green body with dark brown/black matrix and waxy-to-glassy polish; turquoise hardness is Mohs 5–6, typically cryptocrystalline and non-cleavable, with specific gravity about 2.6–2.8.

Formation & geological history

Natural turquoise forms as a secondary copper-aluminum phosphate in arid, oxidized zones of copper deposits, commonly in fractures and breccias; deposits are generally geologically young relative to their host rocks. The specimen is tumbled and may be stabilized, dyed, or reconstituted.

Uses & applications

Used for cabochons, beads, carvings, and collectibles; lower-grade material is often stabilized with resin for durability. It has minor ornamental, not structural, use.

Geological facts

Dark matrix can be limonite, iron oxides, or host rock; uniform vivid color and unusually low price may indicate treatment or imitation. Turquoise is among the oldest known ornamental stones.

Field identification & locations

Common sources include Arizona, Nevada, Iran, China, Chile, and Mexico. Check for natural irregular matrix, moderate hardness, and copper-bearing blue color; avoid destructive tests on polished pieces.