
mineral
Tumbled blue-green stone, possibly dyed turquoise or chrysocolla
Uncertain; turquoise is hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O
AI-generated identification · may be incorrectOpaque blue-green color with a dull-to-waxy luster and rounded tumbled form; apparent hardness is likely about Mohs 3–6, depending on material and treatments. The image is too blurred for reliable identification; it may also be dyed stone or glass.
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Physical properties
Opaque blue-green color with a dull-to-waxy luster and rounded tumbled form; apparent hardness is likely about Mohs 3–6, depending on material and treatments. The image is too blurred for reliable identification; it may also be dyed stone or glass.
Formation & geological history
Natural turquoise forms near-surface in arid copper deposits through weathering and groundwater alteration, commonly during the Cenozoic; chrysocolla forms similarly as a secondary copper mineral. Tumbled specimens are mechanically polished and may be stabilized or dyed.
Uses & applications
Used for cabochons, beads, ornaments, and inexpensive mineral collections; turquoise has longstanding jewelry and cultural significance.
Geological facts
Color alone cannot distinguish turquoise from chrysocolla, dyed howlite, dyed magnesite, or manufactured glass. A diagnostic identification requires close inspection, hardness, streak, magnification, and often chemical testing.
Field identification & locations
Common sources include Iran, the U.S. Southwest, Mexico, Chile, and China. Check for natural matrix, waxy texture, uniform dye concentration, and glass-like translucency; avoid destructive tests on valuable pieces.
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