Rock Identifier
Botryoidal chalcedony (possibly jaspery agate) (Microcrystalline quartz, SiO₂; chalcedony with iron-oxide staining and possible calcite/aragonite inclusions) — mineral
mineral

Botryoidal chalcedony (possibly jaspery agate)

Microcrystalline quartz, SiO₂; chalcedony with iron-oxide staining and possible calcite/aragonite inclusions

AI-generated identification · may be incorrect

White, cream, tan, and rusty-brown specimen with rounded botryoidal surfaces and locally drusy texture; typically waxy to vitreous luster, cryptocrystalline structure, no obvious cleavage, Mohs hardness about 6.5–7, and specific gravity near 2.6.…

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Physical properties

White, cream, tan, and rusty-brown specimen with rounded botryoidal surfaces and locally drusy texture; typically waxy to vitreous luster, cryptocrystalline structure, no obvious cleavage, Mohs hardness about 6.5–7, and specific gravity near 2.6. The porous, bubbly appearance may indicate replacement of a carbonate or cavity lining.

Formation & geological history

Forms when silica-rich groundwater precipitates in cavities, fractures, or porous volcanic/carbonate rock, commonly in successive botryoidal layers; iron oxides create the brown staining. Exact age and locality cannot be determined from the photograph.

Uses & applications

Used as lapidary rough, cabochons, carvings, decorative specimens, and occasionally ornamental stone; this irregular piece has modest commercial value.

Geological facts

Botryoidal means grape-like; each rounded knob can represent a silica growth surface around a cavity or nucleus.

Field identification & locations

Look for waxy translucent edges, conchoidal fracture, very fine texture, and hardness sufficient to scratch ordinary glass. Common sources include Brazil, Uruguay, Mexico, India, and the western United States; acid testing can help detect abundant carbonate but may damage the specimen.