Rock Identifier
Tumbled orange chalcedony (likely carnelian) (Cryptocrystalline quartz, SiO₂; carnelian is orange-red chalcedony colored mainly by iron oxides) — gemstone
gemstone

Tumbled orange chalcedony (likely carnelian)

Cryptocrystalline quartz, SiO₂; carnelian is orange-red chalcedony colored mainly by iron oxides

AI-generated identification · may be incorrect

Typically Mohs hardness 6.5–7, vitreous to waxy luster, translucent orange to reddish-orange color, and no visible cleavage; its microcrystalline quartz structure gives a smooth, tough surface.

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Physical properties

Typically Mohs hardness 6.5–7, vitreous to waxy luster, translucent orange to reddish-orange color, and no visible cleavage; its microcrystalline quartz structure gives a smooth, tough surface.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, later incorporating iron impurities; deposits range from ancient volcanic terrains to younger sedimentary environments.

Uses & applications

Used for beads, cabochons, carvings, seals, and tumbled stones; common polished pieces are inexpensive, while vivid, translucent material has greater jewelry value.

Geological facts

Carnelian is a variety of chalcedony, and heating can intensify its orange-red color. The specimen appears polished or tumbled rather than naturally weathered.

Field identification & locations

Identify it by its uniform orange color, translucency, waxy polish, and lack of cleavage; glass may imitate it but often shows bubbles or a sharper, glassier luster. Common sources include India, Brazil, Uruguay, Madagascar, and Botswana.