
sedimentary
Rounded river cobble, likely weathered sandstone or quartzite
Indeterminate clastic silicate rock; possibly quartz-rich sandstone (SiO₂-dominant)
AI-generated identification · may be incorrectPale 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.
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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.
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