Rock Identifier
Tumbled carnelian (orange chalcedony) (Carnelian, a variety of microcrystalline quartz (SiO₂), often colored by iron oxides) — gemstone
gemstone

Tumbled carnelian (orange chalcedony)

Carnelian, a variety of microcrystalline quartz (SiO₂), often colored by iron oxides

AI-generated identification · may be incorrect

Mohs hardness 6.5–7; translucent orange to reddish-orange, vitreous to waxy luster, cryptocrystalline structure, with no visible cleavage and conchoidal fracture. The rounded, polished shape indicates human processing.

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Physical properties

Mohs hardness 6.5–7; translucent orange to reddish-orange, vitreous to waxy luster, cryptocrystalline structure, with no visible cleavage and conchoidal fracture. The rounded, polished shape indicates human processing.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, with iron producing the orange-red color; deposits range from Paleozoic to Cenozoic in age. Common sources include India, Brazil, Uruguay, Madagascar, and the United States.

Uses & applications

Used for beads, cabochons, carvings, seals, and inexpensive jewelry; tumbled pieces are popular decorative and lapidary specimens.

Geological facts

Carnelian is chalcedony rather than a separate mineral species; heating can intensify its red-orange color. It was widely used for ancient seals and engraved gems.

Field identification & locations

Identify it by its even orange color, translucency, quartz-like hardness, and lack of cleavage; it should scratch glass but not be scratched by a steel blade. Natural banding or agate-like zoning may occur.