Rock Identifier
Tumbled yellow-orange chalcedony (likely carnelian or honey agate) (Microcrystalline quartz, SiO₂; orange coloration commonly from iron oxides) — mineral
mineral

Tumbled yellow-orange chalcedony (likely carnelian or honey agate)

Microcrystalline quartz, SiO₂; orange coloration commonly from iron oxides

AI-generated identification · may be incorrect

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.

Identified More mineral
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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.