Rock Identifier
Polished carnelian agate (Chalcedony (microcrystalline quartz), SiO₂, colored orange-red by iron oxides) — gemstone
gemstone

Polished carnelian agate

Chalcedony (microcrystalline quartz), SiO₂, colored orange-red by iron oxides

AI-generated identification · may be incorrect

Typically Mohs 6.5–7; translucent orange, amber, reddish-brown, or cream with waxy to vitreous luster. Fibrous cryptocrystalline quartz lacks visible cleavage and has conchoidal fracture; the glossy surface appears polished or tumbled.

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Physical properties

Typically Mohs 6.5–7; translucent orange, amber, reddish-brown, or cream with waxy to vitreous luster. Fibrous cryptocrystalline quartz lacks visible cleavage and has conchoidal fracture; the glossy surface appears polished or tumbled.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, with iron staining producing the warm colors; commonly associated with volcanic rocks, usually formed in Phanerozoic volcanic terrains.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and lapidary specimens; durable enough for jewelry and decorative objects.

Geological facts

Carnelian is an orange-red variety of chalcedony, while agate commonly shows banding or color zoning. Heat treatment can intensify its red-orange color.

Field identification & locations

Identify by its translucent warm color, waxy luster, hardness, and conchoidal fracture; common sources include Brazil, India, Uruguay, Madagascar, and the United States. This specimen may be carnelian-rich agate or polished chalcedony.