
mineral
Botryoidal chalcedony (gray agate/jasper-like silica)
Microcrystalline quartz, SiO₂; likely chalcedony with opaque quartz or jasper inclusions
AI-generated identification · may be incorrectTypically Mohs 6.5–7, with a waxy to vitreous luster, gray-white to tan coloration, translucent edges, and curved botryoidal surfaces. It has cryptocrystalline quartz structure, no obvious cleavage, conchoidal fracture, and specific gravity around 2.6.
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Physical properties
Typically Mohs 6.5–7, with a waxy to vitreous luster, gray-white to tan coloration, translucent edges, and curved botryoidal surfaces. It has cryptocrystalline quartz structure, no obvious cleavage, conchoidal fracture, and specific gravity around 2.6.
Formation & geological history
Forms when silica-rich groundwater fills cavities, fractures, or vesicles in volcanic rock and precipitates in successive layers. The specimen’s exact geological age cannot be determined from the image; chalcedony occurs from ancient volcanic terrains to modern deposits.
Uses & applications
Used for ornamental stone, carvings, cabochons, beads, and polished display pieces; massive material is also used decoratively in countertops and architectural objects.
Geological facts
Botryoidal means the surface developed as overlapping rounded growths. Gray chalcedony can resemble weathered limestone, opal, or massive quartz, but its conchoidal fracture and hardness help distinguish it.
Field identification & locations
Look for waxy luster, translucent margins, curved banding or growth layers, and resistance to scratching by steel. Common localities include Brazil, Uruguay, Mexico, India, Madagascar, and volcanic regions worldwide.
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