
mineral
Turquoise-colored rough specimen, possibly dyed howlite or magnesite
Unconfirmed; turquoise is CuAl₆(PO₄)₄(OH)₈·4H₂O, while common turquoise imitations include dyed Ca₂B₅SiO₉(OH)₅ (howlite)
AI-generated identification · may be incorrectOpaque, vivid blue-green, rough and uneven, with a dull to waxy luster. The photo alone cannot establish hardness or crystal structure; turquoise is Mohs 5–6, while howlite is about 3.5.
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Physical properties
Opaque, vivid blue-green, rough and uneven, with a dull to waxy luster. The photo alone cannot establish hardness or crystal structure; turquoise is Mohs 5–6, while howlite is about 3.5.
Formation & geological history
If natural turquoise, it forms through near-surface alteration of aluminum-rich rocks by copper-bearing fluids, commonly in arid regions. Its age depends on the deposit; the specimen’s identity and geological history cannot be confirmed visually.
Uses & applications
Turquoise is used in jewelry and ornament, and as a collectible mineral. Dyed lookalikes are generally inexpensive decorative material.
Geological facts
Color alone is not diagnostic: turquoise, dyed minerals, and imitation materials can look alike. A close examination or gemological test is needed for reliable identification.
Field identification & locations
Natural turquoise commonly occurs in copper deposits in the southwestern United States, Iran, and parts of China. Check for natural-looking color variation and matrix, but use professional testing rather than destructive tests to distinguish imitations.
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