Rock Identifier
Carnelian (orange chalcedony) (Microcrystalline quartz, SiO₂; chalcedony variety colored mainly by iron oxides) — gemstone
gemstone

Carnelian (orange chalcedony)

Microcrystalline quartz, SiO₂; chalcedony variety colored mainly by iron oxides

AI-generated identification · may be incorrect

Typically translucent orange to red-brown with waxy to vitreous luster, conchoidal fracture, and no cleavage; Mohs hardness 6.5–7, trigonal crystal structure at the microscopic level. The pictured piece appears polished or freshly fractured and may be dyed glass or resin if unusually uniform.

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Physical properties

Typically translucent orange to red-brown with waxy to vitreous luster, conchoidal fracture, and no cleavage; Mohs hardness 6.5–7, trigonal crystal structure at the microscopic level. The pictured piece appears polished or freshly fractured and may be dyed glass or resin if unusually uniform.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, with iron producing the orange-red color; deposits occur chiefly in volcanic rocks, commonly Cenozoic to older. Heat treatment can intensify its color.

Uses & applications

Used for beads, cabochons, carvings, seals, and decorative objects; attractive quality has modest jewelry value.

Geological facts

Carnelian is a translucent chalcedony variety, historically used for engraved signet rings and amulets. Its color ranges from pale orange to deep blood-red.

Field identification & locations

Identify by waxy translucence, conchoidal fracture, and hardness sufficient to scratch ordinary glass; glass often shows bubbles and remains softer. Common sources include India, Brazil, Uruguay, Madagascar, and Germany.