Rock Identifier
Quartz-rich pebble, possibly chert or silicified limestone (Microcrystalline quartz (SiO₂), possibly chalcedony; exact identification is uncertain from the photograph) — sedimentary
sedimentary

Quartz-rich pebble, possibly chert or silicified limestone

Microcrystalline quartz (SiO₂), possibly chalcedony; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Small rounded, pale cream-gray specimen with a dull to slightly waxy luster and white curved bands or veins. Likely hardness about 6.5–7 if quartz-rich; cleavage absent, fracture commonly conchoidal; moderate density around 2.6 g/cm³.

Identified More sedimentary
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Physical properties

Small rounded, pale cream-gray specimen with a dull to slightly waxy luster and white curved bands or veins. Likely hardness about 6.5–7 if quartz-rich; cleavage absent, fracture commonly conchoidal; moderate density around 2.6 g/cm³.

Formation & geological history

Probably a weathered river or soil pebble formed by silica cementation, replacement, or chalcedony deposition in sedimentary rocks. The regional setting near 17.2°N, 89.1°W (Petén, Guatemala) commonly exposes limestone and alluvial sediments, making silicified limestone or chert plausible.

Uses & applications

Primarily a curiosity or lapidary material; suitable for tumbling or small cabochons if it cuts cleanly. Not generally used commercially unless present in large deposits.

Geological facts

The pale curved markings may be chalcedony bands, fossil/replacement textures, or weathering surfaces rather than true layering. A steel file should not scratch quartz-rich material, while a knife may scratch softer limestone.

Field identification & locations

Field tests are useful: quartz-rich material scratches glass and does not fizz in dilute hydrochloric acid; calcite-rich limestone fizzes strongly and is softer. Commonly found as stream cobbles and weathered residual fragments in limestone terrains.