
mineral
Tumbled honey-brown chalcedony or agate
Microcrystalline quartz (SiO₂), likely chalcedony; exact identification requires testing
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; translucent honey-yellow to brown, waxy-to-glassy luster, cryptocrystalline structure, and no visible cleavage. The smooth shape indicates tumbling or water wear.
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Physical properties
Hardness about 6.5–7 Mohs; translucent honey-yellow to brown, waxy-to-glassy luster, cryptocrystalline structure, and no visible cleavage. The smooth shape indicates tumbling or water wear.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, precipitating microcrystalline quartz; commonly Cenozoic to older, depending on host rock and locality.
Uses & applications
Used for cabochons, beads, carvings, and small decorative specimens; durable but generally modestly valuable unless strongly colored or patterned.
Geological facts
Chalcedony and agate are varieties of quartz; agate typically shows distinct banding, which is not clearly visible in this specimen.
Field identification & locations
Common in volcanic terrains, river gravels, and silica-rich cavities worldwide, especially Brazil, Uruguay, India, Madagascar, and the western United States. A scratch test, translucency, and absence of cleavage help distinguish it from calcite or glass.
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