Rock Identifier
Botryoidal chalcedony (agate/quartz geode fragment) (Microcrystalline quartz, SiO₂, likely chalcedony with drusy quartz and iron-oxide staining) — mineral
mineral

Botryoidal chalcedony (agate/quartz geode fragment)

Microcrystalline quartz, SiO₂, likely chalcedony with drusy quartz and iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; translucent white to honey-orange/brown, waxy to slightly glassy luster, botryoidal rounded surfaces, no obvious cleavage, conchoidal fracture; quartz crystal structure. The orange-brown color is likely hematite/goethite staining.

Identified More mineral
Explore Botryoidal chalcedony (agate/quartz geode fragment) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness about 6.5–7 Mohs; translucent white to honey-orange/brown, waxy to slightly glassy luster, botryoidal rounded surfaces, no obvious cleavage, conchoidal fracture; quartz crystal structure. The orange-brown color is likely hematite/goethite staining.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rock, depositing successive chalcedony layers and later quartz crystals. Such material is commonly Cenozoic or older depending on its host lava; the image alone cannot establish age.

Uses & applications

Used as a lapidary, cabochon, decorative, and collecting material; polished pieces may be used in jewelry. Small rough specimens have modest commercial value.

Geological facts

The grape-like surface is called botryoidal texture, produced by rounded growth fronts. It may be an exposed cavity lining or a broken fragment of an agate-like nodule.

Field identification & locations

Likely identification is chalcedony/agate rather than a specific species. Test carefully for glassy hardness: it should scratch ordinary glass, while a steel knife generally does not scratch it. In the reported Paraguay region, silica-rich agate and chalcedony are geologically plausible, especially in basalt-associated terrains, though locality confirmation requires the host rock.