Rock Identifier
Rounded gray sandstone or siltstone cobble (Lithified quartz–feldspar–clay sediment; exact petrographic identification requires testing) — sedimentary
sedimentary

Rounded gray sandstone or siltstone cobble

Lithified quartz–feldspar–clay sediment; exact petrographic identification requires testing

AI-generated identification · may be incorrect

Fine-grained, dull to slightly earthy luster, gray-brown color, and weakly visible bedding or weathering lines; estimated Mohs hardness 3–6 depending on cement, with no obvious cleavage. The smooth elongated shape reflects water abrasion rather than crystal structure.

Identified More sedimentary
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Physical properties

Fine-grained, dull to slightly earthy luster, gray-brown color, and weakly visible bedding or weathering lines; estimated Mohs hardness 3–6 depending on cement, with no obvious cleavage. The smooth elongated shape reflects water abrasion rather than crystal structure.

Formation & geological history

Likely deposited as sand or silt, compacted and cemented into sedimentary rock, then rounded in a stream, beach, or glacial environment. Its geological age cannot be determined from the photograph.

Uses & applications

Usually collected as a natural cobble, garden stone, or educational specimen; sandstone may also be used as building or paving stone, though this piece is too small for industry.

Geological facts

The surface appears weathered and possibly slightly porous, consistent with sandstone or siltstone rather than a crystalline igneous rock.

Field identification & locations

Look for gritty texture, visible grains, bedding, and sediment staining; a glass-scratch test, acid test, and hand lens would help distinguish sandstone from siltstone or weathered basalt. Common worldwide in riverbeds, beaches, and sedimentary terrains.