
mineral
Blue-dyed magnesite beads (often sold as “turquoise howlite”)
Magnesite, MgCO₃; commonly dyed blue and possibly marketed as dyed howlite, Ca₂B₅SiO₉(OH)₅
AI-generated identification · may be incorrectPolished spherical beads with pale blue color and brown-gray matrix veining; dull to waxy luster, trigonal carbonate structure, Mohs hardness about 3.5–4.5 (magnesite) or 3–3.5 (howlite), and specific gravity roughly 2.5–3.1.…
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Physical properties
Polished spherical beads with pale blue color and brown-gray matrix veining; dull to waxy luster, trigonal carbonate structure, Mohs hardness about 3.5–4.5 (magnesite) or 3–3.5 (howlite), and specific gravity roughly 2.5–3.1. The color and uniform veining strongly suggest dyeing and stabilization rather than natural turquoise.
Formation & geological history
Magnesite forms by alteration of magnesium-rich rocks and carbonate precipitation; howlite forms in borate-rich evaporite environments. These beads are human-processed, polished, and likely dyed; the source material is generally Cenozoic or older depending on deposit.
Uses & applications
Used for inexpensive jewelry, beads, carvings, and decorative objects. They are turquoise substitutes, not typically valuable gemstones.
Geological facts
Blue dye may concentrate along fractures and wear away at drilled holes or scratched areas. A vinegar or dilute-acid test can fizz on magnesite, but it may damage the finish and is best avoided.
Field identification & locations
Common sources include China, Africa, and the western United States for related magnesite/howlite materials. Check drilled holes for white interiors, test hardness cautiously with a steel needle, and distinguish from turquoise, which is generally harder and more compact.
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