
gemstone
Tumbled carnelian (orange chalcedony)
Carnelian, a microcrystalline variety of quartz (SiO₂), commonly colored by iron oxides
AI-generated identification · may be incorrectTranslucent orange-red, smooth and polished, with waxy to glassy luster and no visible cleavage. Mohs hardness 6.5–7; specific gravity about 2.60–2.65; cryptocrystalline structure.
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Physical properties
Translucent orange-red, smooth and polished, with waxy to glassy luster and no visible cleavage. Mohs hardness 6.5–7; specific gravity about 2.60–2.65; cryptocrystalline structure.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, later acquiring its orange color from iron. It is generally associated with Cenozoic and older volcanic or sedimentary deposits.
Uses & applications
Used for beads, cabochons, carvings, ornaments, and inexpensive jewelry. Small tumbled pieces are usually decorative rather than highly valuable.
Geological facts
The photograph strongly resembles dyed or natural carnelian; color alone cannot confirm which. Natural specimens often show subtle bands, cloudy zones, or uneven translucency.
Field identification & locations
Commonly found in India, Brazil, Uruguay, Madagascar, Germany, and the United States. Check for glass-like hardness, translucency at the edges, and absence of bubbles; a gemological test is needed to distinguish dyed chalcedony or glass.
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