
mineral
Tumbled pale-yellow chalcedony (possibly yellow jasper)
Microcrystalline quartz, SiO₂; chalcedony/jasper varieties
AI-generated identification · may be incorrectSmooth, opaque cream-to-yellow surface with faint banding and brown inclusions; likely Mohs 6.5–7, vitreous to waxy luster, cryptocrystalline quartz structure, no visible cleavage. Specific gravity is typically about 2.6.
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Physical properties
Smooth, opaque cream-to-yellow surface with faint banding and brown inclusions; likely Mohs 6.5–7, vitreous to waxy luster, cryptocrystalline quartz structure, no visible cleavage. Specific gravity is typically about 2.6.
Formation & geological history
Silica-rich fluids deposited quartz in cavities or fractures, later compacted and colored by trace iron oxides; the specimen has been rounded by tumbling. Geological age cannot be determined from the photograph.
Uses & applications
Used as a small ornamental or jewelry stone and collected as a polished specimen; chalcedony is also used for carvings and beads.
Geological facts
Jasper is opaque chalcedony, while more translucent material is generally called chalcedony or agate; the image alone cannot distinguish these reliably.
Field identification & locations
The rounded polish and faint internal color variation fit tumbled chalcedony. Quartz-rich rocks occur in the western North Carolina region, but this small processed piece cannot be tied to a local source by appearance alone.
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