Rock Identifier
Botryoidal chalcedony (possibly agate/geode material) (Microcrystalline quartz, SiO₂; commonly chalcedony with quartz-lined cavities and iron-oxide staining) — mineral
mineral

Botryoidal chalcedony (possibly agate/geode material)

Microcrystalline quartz, SiO₂; commonly chalcedony with quartz-lined cavities and iron-oxide staining

AI-generated identification · may be incorrect

White, cream, tan, and brown rounded botryoidal surfaces with waxy to dull luster and small sparkling quartz druses. Hardness about 6.5–7 Mohs, no cleavage, conchoidal fracture, cryptocrystalline structure; specific gravity about 2.58–2.64.

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Physical properties

White, cream, tan, and brown rounded botryoidal surfaces with waxy to dull luster and small sparkling quartz druses. Hardness about 6.5–7 Mohs, no cleavage, conchoidal fracture, cryptocrystalline structure; specific gravity about 2.58–2.64.

Formation & geological history

Forms when silica-rich groundwater fills cavities or vesicles in volcanic rock, depositing concentric chalcedony layers and later quartz crystals; iron oxides create the brown coloration. Formation is generally Cenozoic to older, depending on the host rock.

Uses & applications

Used as a lapidary, carving, ornamental, and display material; attractive pieces may be polished or cut into cabochons. Ordinary specimens have modest commercial value.

Geological facts

The rounded “grape-like” texture is called botryoidal growth and develops from repeated silica precipitation around nucleation points.

Field identification & locations

Identify by its very hard, glassy fracture, inability to scratch with a steel knife, and waxy chalcedony texture; acid should not fizz. Similar material occurs in volcanic regions worldwide, including Brazil, Mexico, Uruguay, India, and the western United States.