Rock Identifier
Botryoidal chalcedony (gray agate/jasper-like silica) (Microcrystalline quartz, SiO₂; likely chalcedony with opaque quartz or jasper inclusions) — mineral
mineral

Botryoidal chalcedony (gray agate/jasper-like silica)

Microcrystalline quartz, SiO₂; likely chalcedony with opaque quartz or jasper inclusions

AI-generated identification · may be incorrect

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.

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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.