
mineral
Blue-green turquoise-like tumbled stone
Turquoise, hydrous copper aluminum phosphate: CuAl₆(PO₄)₄(OH)₈·4H₂O
AI-generated identification · may be incorrectAppears opaque blue-green with a matte-to-waxy luster and rounded, polished edges. Turquoise has Mohs hardness 5–6, cryptocrystalline structure, no prominent cleavage, and specific gravity about 2.6–2.9; the blurred image prevents confident confirmation.
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Physical properties
Appears opaque blue-green with a matte-to-waxy luster and rounded, polished edges. Turquoise has Mohs hardness 5–6, cryptocrystalline structure, no prominent cleavage, and specific gravity about 2.6–2.9; the blurred image prevents confident confirmation.
Formation & geological history
Forms as a secondary mineral in arid regions when copper-rich groundwater alters aluminum- and phosphorus-bearing rocks, commonly in fractures and breccias. Deposits are generally geologically young relative to their host rocks, often associated with weathering zones.
Uses & applications
Used as a gemstone in cabochons, beads, carvings, and jewelry; lower-grade material is used for ornamental objects and occasionally stabilized or reconstituted products.
Geological facts
Natural turquoise commonly shows brown or black limonite/iron-manganese matrix, though none is clearly visible here. Similar blue-green materials include dyed howlite, chrysocolla, amazonite, and glass.
Field identification & locations
Common localities include Iran, Arizona and Nevada, China, Mexico, Chile, and Egypt. Field tests include checking for opaque color, waxy luster, hardness, and matrix; avoid destructive tests because treated imitations are common.
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