
mineral
Tumbled chalcedony (likely carnelian or yellow jasper)
Microcrystalline quartz, SiO₂; iron-oxide-bearing chalcedony/jasper
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; cream, honey-yellow, orange, and reddish-brown mottling; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6. The rounded, glossy surface indicates tumbling and polishing.
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Physical properties
Hardness 6.5–7 Mohs; cream, honey-yellow, orange, and reddish-brown mottling; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6. The rounded, glossy surface indicates tumbling and polishing.
Formation & geological history
Silica-rich groundwater deposited microcrystalline quartz in cavities or fractures, with iron oxides producing the warm colors; such material commonly formed in volcanic rocks during the Cenozoic or earlier. The exact geological age and locality cannot be determined from the photograph.
Uses & applications
Used for beads, cabochons, carvings, decorative objects, and inexpensive jewelry; jasper and chalcedony are also used as ornamental stone.
Geological facts
Color variation reflects hematite/goethite staining; translucent edges would favor chalcedony or carnelian, while opaque areas favor jasper.
Field identification & locations
Identify with a glass-scratching test, absence of cleavage, waxy luster, and iron-rich banding or patches; common sources include Brazil, India, Madagascar, Uruguay, and the western United States.
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