Rock Identifier
Tumbled yellow chalcedony or calcite (Cryptocrystalline quartz (SiO₂), possibly yellow chalcedony; an alternative is yellow calcite (CaCO₃)) — mineral
mineral

Tumbled yellow chalcedony or calcite

Cryptocrystalline quartz (SiO₂), possibly yellow chalcedony; an alternative is yellow calcite (CaCO₃)

AI-generated identification · may be incorrect

Smooth, rounded, cream-yellow, and waxy to weakly vitreous; chalcedony has Mohs hardness 6.5–7 and no cleavage, while calcite is softer (Mohs 3) with rhombohedral cleavage. The opaque, cloudy appearance prevents confident identification from the image alone.

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Physical properties

Smooth, rounded, cream-yellow, and waxy to weakly vitreous; chalcedony has Mohs hardness 6.5–7 and no cleavage, while calcite is softer (Mohs 3) with rhombohedral cleavage. The opaque, cloudy appearance prevents confident identification from the image alone.

Formation & geological history

Yellow chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; calcite forms from carbonate-rich fluids or sedimentary deposits. Both range from ancient to geologically recent and may be naturally rounded or mechanically tumbled.

Uses & applications

Used as a decorative tumbled stone, cabochon, paperweight, and collector specimen; chalcedony can be used in jewelry, whereas calcite is generally less durable.

Geological facts

A steel knife or glass-scratch test can help distinguish them: chalcedony resists scratching and may scratch glass; calcite scratches easily. Dilute vinegar or acid fizzes on calcite but not chalcedony, though testing can damage the specimen.

Field identification & locations

Common sources include Brazil, Mexico, India, Madagascar, and the United States. Confirm identity with hardness, acid reaction, and ideally specific gravity or microscopy.