Rock Identifier
Tumbled yellow chalcedony (likely yellow agate or common opal) (Microcrystalline quartz, SiO₂ (chalcedony/agate); exact identification requires testing) — mineral
mineral

Tumbled yellow chalcedony (likely yellow agate or common opal)

Microcrystalline quartz, SiO₂ (chalcedony/agate); exact identification requires testing

AI-generated identification · may be incorrect

Honey-yellow to cream, translucent, waxy-to-glassy luster, curved fracture, and no visible cleavage; chalcedony hardness is about 6.5–7 Mohs, while common opal is 5.5–6.5. The polished surface and rounded shape indicate human tumbling.

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Physical properties

Honey-yellow to cream, translucent, waxy-to-glassy luster, curved fracture, and no visible cleavage; chalcedony hardness is about 6.5–7 Mohs, while common opal is 5.5–6.5. The polished surface and rounded shape indicate human tumbling.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, often in volcanic rocks; agate develops from successive silica deposition. Common opal forms from hydrated silica gel; formation ages range from recent to ancient depending on the host rock.

Uses & applications

Used for beads, cabochons, carvings, ornaments, and lapidary practice; attractive translucent pieces have modest jewelry value.

Geological facts

The specimen may be dyed or heat-treated, though its warm color can also be natural. A refractive-index, specific-gravity, and water-absorption test can distinguish chalcedony from opal.

Field identification & locations

Common sources include Brazil, Uruguay, Mexico, Madagascar, Australia, and the western United States. Field clues are translucency, waxy luster, conchoidal fracture, and absence of cleavage; a scratch test should be done inconspicuously.