Rock Identifier
Polished carnelian agate cabochon (Microcrystalline quartz (chalcedony), SiO₂, colored mainly by iron oxides) — gemstone
gemstone

Polished carnelian agate cabochon

Microcrystalline quartz (chalcedony), SiO₂, colored mainly by iron oxides

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent orange-red to reddish brown, vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, specific gravity about 2.58–2.64. The oval cabochon appears polished and may contain natural pits or inclusions.

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Physical properties

Hardness 6.5–7 Mohs; translucent orange-red to reddish brown, vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, specific gravity about 2.58–2.64. The oval cabochon appears polished and may contain natural pits or inclusions.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, with iron producing the orange-red color; commonly Cenozoic to older, depending on its host rock. It is found worldwide, notably in India, Brazil, Uruguay, Madagascar, Botswana, and the United States.

Uses & applications

Used for beads, cabochons, carvings, seals, and ornamental objects; durable enough for jewelry but less valuable than fine transparent gems.

Geological facts

Carnelian is an orange-red variety of chalcedony and grades into sard when darker brown-red. Strong, even color and translucency generally increase desirability.

Field identification & locations

Identify by its waxy luster, translucency, lack of cleavage, and hardness sufficient to scratch glass; natural banding may be subtle. This specimen’s bright, uniform color and rounded polish could also indicate heat treatment or dye enhancement.