Rock Identifier
Orange chalcedony (possibly carnelian) (Microcrystalline quartz, SiO₂; orange chalcedony is commonly called carnelian) — mineral
mineral

Orange chalcedony (possibly carnelian)

Microcrystalline quartz, SiO₂; orange chalcedony is commonly called carnelian

AI-generated identification · may be incorrect

Opaque to translucent orange-yellow with a waxy luster and irregular fracture; quartz hardness is 7 Mohs, trigonal crystal structure at microscopic scale, with no cleavage. The surface appears naturally worn, though the image alone cannot confirm whether it has been polished or treated.

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Physical properties

Opaque to translucent orange-yellow with a waxy luster and irregular fracture; quartz hardness is 7 Mohs, trigonal crystal structure at microscopic scale, with no cleavage. The surface appears naturally worn, though the image alone cannot confirm whether it has been polished or treated.

Formation & geological history

Silica-rich fluids deposited quartz in rock cavities or fractures; iron compounds commonly create the orange color. Chalcedony forms in many geological settings and spans a broad range of ages.

Uses & applications

Used for beads, cabochons, carvings, and ornamental objects; chalcedony also has limited industrial uses as silica material.

Geological facts

Carnelian is a traditional variety name for red-to-orange chalcedony; color can be enhanced by heating or dyeing.

Field identification & locations

Look for a smooth, waxy surface, conchoidal fracture, and hardness sufficient to scratch glass; common sources include India, Brazil, Uruguay, and Madagascar. Identification as carnelian rather than another orange stone needs closer inspection.