
mineral
Tumbled yellow-orange chalcedony (likely carnelian or honey agate)
Microcrystalline quartz, SiO₂; orange coloration commonly from iron oxides
AI-generated identification · may be incorrectMohs hardness 6.5–7; translucent yellow-orange to reddish coloration, waxy-to-glassy luster, conchoidal fracture, no cleavage, and quartz’s trigonal crystal structure. The smooth shape indicates tumbling and polishing.
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Physical properties
Mohs hardness 6.5–7; translucent yellow-orange to reddish coloration, waxy-to-glassy luster, conchoidal fracture, no cleavage, and quartz’s trigonal crystal structure. The smooth shape indicates tumbling and polishing.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures, depositing cryptocrystalline quartz over long periods; iron oxidation produces the warm colors. Such material occurs in volcanic and sedimentary host rocks, generally from relatively young to ancient deposits.
Uses & applications
Used for beads, cabochons, ornaments, and inexpensive decorative stones; polished pieces are popular in mineral collections.
Geological facts
Carnelian is the red-orange variety of chalcedony, while paler yellow material may be called honey chalcedony or agate depending on banding and translucency.
Field identification & locations
Identify by its very hard, smooth, quartz-like surface and inability to scratch with a steel nail; it should scratch glass but not be scratched by it. Common sources include India, Brazil, Madagascar, Uruguay, and the United States.
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