Rock Identifier
Polished pink-orange chalcedony (likely carnelian) (Microcrystalline quartz, SiO₂; carnelian is orange-red chalcedony) — mineral
mineral

Polished pink-orange chalcedony (likely carnelian)

Microcrystalline quartz, SiO₂; carnelian is orange-red chalcedony

AI-generated identification · may be incorrect

Translucent to opaque, smooth polished surface with a waxy-to-vitreous luster; quartz hardness 6.5–7, trigonal crystal structure, no cleavage. The image does not reveal internal banding or other diagnostic features.

Identified More mineral
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Physical properties

Translucent to opaque, smooth polished surface with a waxy-to-vitreous luster; quartz hardness 6.5–7, trigonal crystal structure, no cleavage. The image does not reveal internal banding or other diagnostic features.

Formation & geological history

Chalcedony forms as silica-rich fluids fill cavities and fractures, commonly in volcanic rocks; iron oxides produce orange-red colors. Deposits form across many geological ages.

Uses & applications

Used for beads, cabochons, carvings, and decorative objects; chalcedony is also collected as a lapidary material.

Geological facts

Carnelian is a traditional variety of chalcedony, but visual identification from a small photograph is not definitive.

Field identification & locations

Look for hardness, waxy luster, and—where present—translucency or banding; common sources include India, Brazil, and Uruguay. This appears to be a small polished piece.