
mineral
Polished multicolored stone bead bracelet
Likely dyed or treated agate/jasper, chiefly microcrystalline quartz (SiO₂)
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; rounded, polished beads with opaque to translucent red, green, gray, and cream bands or patches; waxy to glassy luster and no visible cleavage. Exact mineral identity is uncertain because the beads appear strongly dyed or composite-treated.
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Physical properties
Hardness about 6.5–7 Mohs; rounded, polished beads with opaque to translucent red, green, gray, and cream bands or patches; waxy to glassy luster and no visible cleavage. Exact mineral identity is uncertain because the beads appear strongly dyed or composite-treated.
Formation & geological history
Agate and jasper form when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks, developing layered chalcedony over long geological periods. The beads were later cut, drilled, polished, and possibly dyed or coated by humans.
Uses & applications
Used primarily for inexpensive jewelry, decorative crafts, and beadwork; commercial value is generally modest.
Geological facts
The vivid, repeated colors and surface appearance are consistent with treated commercial agate, jasper, or reconstructed stone rather than a single identifiable natural rock.
Field identification & locations
Check for natural banding, color concentrated in cracks or drill holes, dye rubbing, and uniformity between beads; a glass or steel scratch test should be avoided on finished jewelry. Similar material is commonly sold from China, India, Brazil, and Madagascar.
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