
mineral
Turquoise-colored bead necklace (likely dyed howlite or magnesite)
Likely dyed Ca₂B₅SiO₉(OH)₅ (howlite) or MgCO₃ (magnesite); turquoise is CuAl₆(PO₄)₄(OH)₈·4H₂O
AI-generated identification · may be incorrectOpaque bright blue beads with dark web-like veining and a polished surface. The image cannot confirm the material; genuine turquoise is Mohs 5–6, while howlite is about 3.5 and magnesite about 3.5–4.5.
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Physical properties
Opaque bright blue beads with dark web-like veining and a polished surface. The image cannot confirm the material; genuine turquoise is Mohs 5–6, while howlite is about 3.5 and magnesite about 3.5–4.5.
Formation & geological history
The beads appear to imitate turquoise; howlite and magnesite form in evaporite or borate-rich deposits and are often dyed and shaped for jewelry. Genuine turquoise forms secondarily in oxidized copper deposits.
Uses & applications
Used as jewelry; comparable beads may be made from turquoise, dyed howlite, or dyed magnesite.
Geological facts
The vivid, unusually uniform blue and dark matrix are common in dyed turquoise simulants, but appearance alone is not definitive.
Field identification & locations
A scratch, magnification, or laboratory test can help distinguish materials; avoid damaging the beads. Howlite and magnesite are common in North America, while turquoise sources include Iran, the southwestern United States, and China.
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