
mineral
Tumbled carnelian
Carnelian, a red-orange variety of microcrystalline chalcedony (SiO₂)
AI-generated identification · may be incorrectMohs hardness 6.5–7; translucent orange-brown body with darker inclusions, vitreous to waxy luster, cryptocrystalline quartz, and no visible cleavage. Its smooth rounded shape indicates tumbling and polishing.
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Physical properties
Mohs hardness 6.5–7; translucent orange-brown body with darker inclusions, vitreous to waxy luster, cryptocrystalline quartz, and no visible cleavage. Its smooth rounded shape indicates tumbling and polishing.
Formation & geological history
Forms when iron impurities color chalcedony in silica-rich volcanic cavities, veins, or sedimentary deposits; the material may be millions to hundreds of millions of years old. Common sources include India, Brazil, Uruguay, Madagascar, and Botswana.
Uses & applications
Used for beads, cabochons, carvings, seals, and ornamental objects; durable polished pieces are popular in jewelry and mineral collections.
Geological facts
Carnelian’s color ranges from yellow-orange to deep reddish brown and can darken with heating. Ancient Egyptians, Greeks, Romans, and Mesopotamians used it for amulets and engraved gems.
Field identification & locations
Identify it by its uniform orange-red chalcedony color, translucency, quartz hardness, and absence of cleavage; it should scratch glass but not be scratched by a steel blade. Dark spots may be iron-rich inclusions or pits.
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