
mineral
Chalcedony (gray-white agate)
Microcrystalline quartz, SiO₂
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent white, gray, and pale tan with a waxy to vitreous luster. Fibrous cryptocrystalline quartz, generally without cleavage, with conchoidal fracture; specific gravity about 2.6.
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Physical properties
Hardness 6.5–7 Mohs; translucent white, gray, and pale tan with a waxy to vitreous luster. Fibrous cryptocrystalline quartz, generally without cleavage, with conchoidal fracture; specific gravity about 2.6.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, precipitating in microscopic quartz fibers; commonly associated with Cenozoic volcanic terrains, though individual specimens may be much younger.
Uses & applications
Used for cabochons, beads, carvings, lapidary slabs, and ornamental objects; durable varieties are also used as decorative stone. Common pieces typically have modest collector value.
Geological facts
The cloudy, layered appearance and waxy surface are characteristic of chalcedony; more distinctly banded material is called agate, while drusy cavities may contain quartz crystals.
Field identification & locations
Identify it by its translucent edges, smooth waxy luster, hardness, and conchoidal fracture; it should scratch glass but not be scratched by a steel knife. Common localities include Brazil, Uruguay, Mexico, India, Namibia, and the western United States.
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