
mineral
Blue-and-white polished stone, likely dyed howlite or turquoise imitation
Probably dyed magnesite/howlite (CaCO₃), but the image is insufficient for confirmation
AI-generated identification · may be incorrectOpaque sky-blue material with white/gray veining, waxy to glassy polish, and irregular tumbled form. If howlite or magnesite, hardness is about 3–4 Mohs; genuine turquoise is harder, about 5–6, with a cryptocrystalline structure and no visible cleavage.
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Physical properties
Opaque sky-blue material with white/gray veining, waxy to glassy polish, and irregular tumbled form. If howlite or magnesite, hardness is about 3–4 Mohs; genuine turquoise is harder, about 5–6, with a cryptocrystalline structure and no visible cleavage.
Formation & geological history
Howlite and magnesite form in borate- or carbonate-rich sedimentary environments; blue dye is commonly added after cutting or tumbling. Genuine turquoise forms by secondary alteration of copper-bearing rocks, generally in arid regions, over geologically recent hydrothermal-weathering stages.
Uses & applications
Commonly used for inexpensive beads, cabochons, carvings, and worry stones; turquoise is also used in jewelry and has higher value. Dyed substitutes have modest decorative value.
Geological facts
Strongly vivid, evenly distributed blue color and white spiderweb-like veining often indicate dyed howlite or magnesite rather than natural turquoise. A definitive identification requires hardness, density, magnification, and dye testing.
Field identification & locations
Common sources of dyed material include China and India; turquoise occurs in Arizona, Nevada, Iran, Tibet, and Mexico. Check for dye concentration in cracks, a relatively soft scratch response, and a white streak; avoid destructive tests on polished pieces.
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