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

Tumbled carnelian (orange chalcedony)

Carnelian, a cryptocrystalline variety of quartz (SiO₂), colored mainly by dispersed iron oxides

AI-generated identification · may be incorrect

Typically translucent orange to reddish-orange with a waxy to glassy luster; hardness 6.5–7 Mohs, no visible crystal faces, conchoidal fracture, and specific gravity about 2.6. The smooth rounded shape indicates tumbling and polishing.

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Physical properties

Typically translucent orange to reddish-orange with a waxy to glassy luster; hardness 6.5–7 Mohs, no visible crystal faces, conchoidal fracture, and specific gravity about 2.6. The smooth rounded shape indicates tumbling and polishing.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, with iron impurities producing the orange color; commonly associated with volcanic rocks and ancient sediments. Deposits range from Precambrian to recent geological ages.

Uses & applications

Used for beads, cabochons, carvings, seals, and ornamental objects; durable enough for everyday jewelry. Common tumbled pieces have modest value.

Geological facts

Carnelian is closely related to sard, with color determined largely by iron content and heat treatment. Ancient Egyptians and Romans widely used it in amulets and engraved seals.

Field identification & locations

Found commonly in India, Brazil, Uruguay, Madagascar, and Germany. Identify it by its orange-red translucent body, uniform waxy appearance, quartz hardness, and lack of cleavage; this specimen’s exact identity is image-based.