Rock Identifier
Tumbled carnelian agate (Cryptocrystalline quartz (SiO₂), chalcedony variety with iron-oxide coloration) — gemstone
gemstone

Tumbled carnelian agate

Cryptocrystalline quartz (SiO₂), chalcedony variety with iron-oxide coloration

AI-generated identification · may be incorrect

Mohs hardness 6.5–7; translucent orange-red to brown with cream chalcedony bands, waxy to vitreous luster, and no visible cleavage. Its rounded shape and glossy surface indicate mechanical tumbling and polishing.

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Physical properties

Mohs hardness 6.5–7; translucent orange-red to brown with cream chalcedony bands, waxy to vitreous luster, and no visible cleavage. Its rounded shape and glossy surface indicate mechanical tumbling and polishing.

Formation & geological history

Silica-rich groundwater filled cavities in volcanic rock, forming chalcedony; iron oxides produced the red-orange color. Agates commonly formed in Paleozoic–Cenozoic volcanic environments, though the specimen’s exact age cannot be determined visually.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and inexpensive jewelry; polished pieces are popular collectors’ specimens.

Geological facts

Carnelian is the orange-red variety of chalcedony; paler material may be heat-treated to intensify its color. The cream-red pattern suggests agate or jasper-like chalcedony rather than pure carnelian.

Field identification & locations

Identify by its waxy luster, hardness, translucency, conchoidal fracture, and lack of cleavage; common sources include Brazil, Uruguay, India, Madagascar, and Botswana. A steel blade should not easily scratch it, while quartz can scratch glass.