Rock Identifier
Rounded gray-brown cobble, likely weathered sandstone or quartzite (Tentatively quartz-rich sandstone (SiO₂-dominated); exact identification requires hardness and acid tests) — sedimentary
sedimentary

Rounded gray-brown cobble, likely weathered sandstone or quartzite

Tentatively quartz-rich sandstone (SiO₂-dominated); exact identification requires hardness and acid tests

AI-generated identification · may be incorrect

Fine-grained, dull to weakly earthy luster, tan-brown weathering rind, gray interior, and rounded water-worn form; likely hardness ~6–7 if quartz-rich, with no obvious cleavage. The photograph does not resolve grain size or cement confidently.

Identified More sedimentary
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Physical properties

Fine-grained, dull to weakly earthy luster, tan-brown weathering rind, gray interior, and rounded water-worn form; likely hardness ~6–7 if quartz-rich, with no obvious cleavage. The photograph does not resolve grain size or cement confidently.

Formation & geological history

Probably transported and rounded by stream, river, or beach abrasion; the original rock may have formed from lithified sand, potentially hundreds of millions of years old. A metamorphosed equivalent would be quartzite, so classification remains provisional.

Uses & applications

Common sandstone is used as building stone, paving, aggregate, and landscaping material; attractive pieces may be collected as natural specimens. This ordinary cobble has little commercial value.

Geological facts

Quartz-rich sandstone and quartzite can look similar in photographs. A steel nail or knife should not readily scratch quartzite, while dilute hydrochloric acid should not visibly fizz unless carbonate cement is present.

Field identification & locations

Look for visible sand grains, bedding, and a gritty texture for sandstone; quartzite is typically harder, more crystalline, and fractures across grains. Common worldwide in river gravels, beaches, and eroded sedimentary terrains.