
mineral
Raw turquoise
Turquoise, CuAl6(PO4)4(OH)8·4H2O; likely turquoise-bearing rock with pale host matrix
AI-generated identification · may be incorrectHydrated copper-aluminum phosphate; typically blue-green, waxy to dull luster, cryptocrystalline, opaque, and Mohs hardness 5–6. The specimen shows pale green-blue color, brown-gray matrix, and irregular fracture; its exact identity cannot be confirmed from an image alone.
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Physical properties
Hydrated copper-aluminum phosphate; typically blue-green, waxy to dull luster, cryptocrystalline, opaque, and Mohs hardness 5–6. The specimen shows pale green-blue color, brown-gray matrix, and irregular fracture; its exact identity cannot be confirmed from an image alone.
Formation & geological history
Forms as a secondary mineral in arid, oxidized zones of copper deposits when phosphate-bearing groundwater alters aluminum-rich rocks. Most turquoise is geologically young, commonly Cenozoic, though deposits may be older.
Uses & applications
Used as a gemstone, cabochon, bead, carving, and collector specimen; gem quality is commonly stabilized with resin. It has little construction or industrial use.
Geological facts
Color varies with copper, iron, and zinc content: greener material may contain more iron or zinc. Natural turquoise is porous and can darken or absorb oils, solvents, and moisture.
Field identification & locations
Common localities include Iran, the southwestern United States, China, Egypt, Chile, and Mexico. A field clue is blue-green color in a soft, opaque, veined mass associated with limonite or other matrix; avoid confusing dyed howlite or magnesite with turquoise.
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