
mineral
Polished orange chalcedony pendant
Chalcedony, microcrystalline quartz (SiO₂), likely orange carnelian or orange agate
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; peach-orange, translucent to opaque, waxy-to-glassy luster, cryptocrystalline quartz with no visible cleavage. The specimen is polished and wire-wrapped in metal.
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Physical properties
Hardness 6.5–7 Mohs; peach-orange, translucent to opaque, waxy-to-glassy luster, cryptocrystalline quartz with no visible cleavage. The specimen is polished and wire-wrapped in metal.
Formation & geological history
Silica-rich groundwater deposited quartz fibers in cavities or fractures, commonly in volcanic rocks; coloration generally comes from iron oxides. Chalcedony forms across many geological ages, often in Cenozoic volcanic environments.
Uses & applications
Used for cabochons, pendants, beads, carvings, and ornamental objects; durable and affordable jewelry material.
Geological facts
Carnelian is typically uniformly orange-red, while agate shows banding or contrasting zones; the visible subtle zoning may indicate agate/chalcedony rather than solid carnelian.
Field identification & locations
Common sources include Brazil, Uruguay, India, Madagascar, Germany, and the western United States. Identify by its waxy appearance, translucency, hardness, and lack of cleavage; glass imitations may show bubbles or scratch more easily.