Rock Identifier
Botryoidal chalcedony (possibly common opal) (Microcrystalline quartz, SiO₂; pale portions may include hydrated silica opal, SiO₂·nH₂O) — mineral
mineral

Botryoidal chalcedony (possibly common opal)

Microcrystalline quartz, SiO₂; pale portions may include hydrated silica opal, SiO₂·nH₂O

AI-generated identification · may be incorrect

White to translucent, rounded botryoidal surfaces with a waxy to vitreous luster; quartz hardness about 6.5–7 Mohs, opal about 5.5–6.5. No visible cleavage; cryptocrystalline or amorphous structure and typically low-to-moderate specific gravity (about 2.0–2.65).

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Physical properties

White to translucent, rounded botryoidal surfaces with a waxy to vitreous luster; quartz hardness about 6.5–7 Mohs, opal about 5.5–6.5. No visible cleavage; cryptocrystalline or amorphous structure and typically low-to-moderate specific gravity (about 2.0–2.65).

Formation & geological history

Forms when silica-rich groundwater deposits successive layers in cavities, fractures, or vesicles, commonly in volcanic rocks; specimens may range from ancient to recent depending on the host deposit.

Uses & applications

Used as a lapidary stone, cabochon, carving material, and collectible specimen; translucent colorful varieties may be sold as gemstone material.

Geological facts

The bubble-like texture is called botryoidal, meaning grape-shaped. Its appearance can resemble white chalcedony, common opal, or chalcedony coating a porous host.

Field identification & locations

Look for hardness above glass, conchoidal fracture, waxy luster, and lack of fizz in dilute acid; a loupe may reveal translucent chalcedony layers. Common sources include volcanic regions in the western United States, Mexico, Brazil, Turkey, and Australia.