
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 incorrectOpaque 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.
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