
sedimentary
Weathered quartz-rich sandstone or quartzite cobble
Quartz arenite sandstone; possibly weakly metamorphosed quartzite, composed mainly of SiO₂ (quartz)
AI-generated identification · may be incorrectHardness about 6–7; pale gray-beige, fine-grained, dull to slightly granular luster, massive structure, and no obvious cleavage. The rounded form and faint horizontal bands suggest water-worn bedding or compositional layering.
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Physical properties
Hardness about 6–7; pale gray-beige, fine-grained, dull to slightly granular luster, massive structure, and no obvious cleavage. The rounded form and faint horizontal bands suggest water-worn bedding or compositional layering.
Formation & geological history
Likely lithified quartz-rich sand deposited in an ancient river, beach, or marine setting, later uplifted and rounded by erosion; age cannot be determined from the image. If quartzite, burial and metamorphism recrystallized the sandstone.
Uses & applications
Common sandstone is used for building stone, paving, aggregate, and landscaping; quartzite is used for durable countertops, roadstone, and decorative stone. This individual cobble has little commercial value.
Geological facts
Its smooth, elliptical shape indicates prolonged transport or mechanical weathering. The pale color reflects abundant quartz and limited dark iron-bearing minerals.
Field identification & locations
Common in stream gravels, glacial deposits, beaches, and landscaping beds. Test with a steel nail and inspect a fresh break: quartzite resists scratching and fractures across grains, while sandstone commonly breaks around visible sand grains.
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