
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 incorrectWhite, 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.
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