Rock Identifier
Orange chalcedony or carnelian fragment (Microcrystalline quartz, SiO₂; carnelian is orange cryptocrystalline quartz colored mainly by iron oxides) — gemstone
gemstone

Orange chalcedony or carnelian fragment

Microcrystalline quartz, SiO₂; carnelian is orange cryptocrystalline quartz colored mainly by iron oxides

AI-generated identification · may be incorrect

Typically Mohs hardness 6.5–7, translucent to opaque, orange-red, with a waxy to vitreous luster and no visible cleavage; conchoidal fracture is common. The angular piece appears roughly knapped or naturally fractured, though the image is insufficient for certainty.

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Physical properties

Typically Mohs hardness 6.5–7, translucent to opaque, orange-red, with a waxy to vitreous luster and no visible cleavage; conchoidal fracture is common. The angular piece appears roughly knapped or naturally fractured, though the image is insufficient for certainty.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, later depositing cryptocrystalline quartz; iron oxidation produces the orange-red color. Chalcedony occurs in volcanic rocks and sedimentary environments, generally ranging from Paleozoic to recent formations.

Uses & applications

Used for beads, cabochons, carvings, seals, and ornamental objects; lower-grade material is inexpensive and decorative.

Geological facts

Carnelian is the orange-red variety of chalcedony, while paler orange material may be called orange chalcedony. Color can be enhanced by heating or dyeing.

Field identification & locations

Common sources include India, Brazil, Uruguay, Madagascar, and the United States. Field clues are hardness, waxy luster, uniform fine texture, and conchoidal fracture; glass can look similar but often shows bubbles or sharper vitreous luster.