
mineral
Turquoise-look beads, likely dyed howlite or magnesite
Often dyed CaCO₃ (howlite/magnesite), rather than natural turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O
AI-generated identification · may be incorrectBlue-green, opaque, waxy to dull luster with dark spiderweb veining; bead surfaces are polished and spherical. Howlite has Mohs hardness 3–3.5, magnesite 3.5–4, and turquoise 5–6; all are nonmetallic and lack visible crystal faces.
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Physical properties
Blue-green, opaque, waxy to dull luster with dark spiderweb veining; bead surfaces are polished and spherical. Howlite has Mohs hardness 3–3.5, magnesite 3.5–4, and turquoise 5–6; all are nonmetallic and lack visible crystal faces.
Formation & geological history
Howlite and magnesite form as secondary carbonate minerals in sedimentary or hydrothermal environments and are commonly dyed to imitate turquoise; their exact geological age depends on the deposit. Natural turquoise forms in arid, copper-rich oxidation zones.
Uses & applications
Used primarily for inexpensive jewelry, beads, carvings, and decorative objects; genuine turquoise has additional collector and fine-jewelry value.
Geological facts
The unusually uniform color and dense black veining strongly suggest dyed howlite or magnesite (“turquenite”), not high-grade natural turquoise. Dye may concentrate in cracks and can bleed with solvents.
Field identification & locations
Check inconspicuous areas for white interiors, dye pooling, or acetone transfer; a hardness test should be done only on an inconspicuous spot. Common sources include China, Africa, and the United States for turquoise-look material.
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