Rock Identifier
Rounded river cobble, likely weathered sandstone or quartzite (Indeterminate clastic silicate rock; possibly quartz-rich sandstone (SiO₂-dominant)) — sedimentary
sedimentary

Rounded river cobble, likely weathered sandstone or quartzite

Indeterminate clastic silicate rock; possibly quartz-rich sandstone (SiO₂-dominant)

AI-generated identification · may be incorrect

Pale tan-gray, massive, fine-grained, dull to slightly earthy luster, with rounded abrasion surfaces and minor fractures. Estimated hardness is ~6–7 if quartz-rich; cleavage is absent and specific gravity roughly 2.5–2.7.

Identified More sedimentary
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Physical properties

Pale tan-gray, massive, fine-grained, dull to slightly earthy luster, with rounded abrasion surfaces and minor fractures. Estimated hardness is ~6–7 if quartz-rich; cleavage is absent and specific gravity roughly 2.5–2.7.

Formation & geological history

Likely formed as a sedimentary clastic rock and later rounded by transport in a river or beach environment; exact geological age and origin cannot be determined from the photograph.

Uses & applications

Common cobbles are used for landscaping, drainage, decorative stone, and educational collections; this specimen has little commercial or jewelry value unless testing reveals an unusual composition.

Geological facts

Its smooth, subdued shape indicates prolonged mechanical weathering and abrasion rather than crystal growth. The small dark inclusions may be iron oxides, lithic grains, or surface debris.

Field identification & locations

Field identification requires a fresh surface, hand lens, streak, and acid test: quartz-rich material is hard, does not scratch with a steel knife, and shows no fizz with dilute hydrochloric acid. Similar cobbles occur in river gravels worldwide.