
sedimentary
Weathered sandstone or iron-stained quartzite pebble
Likely quartz-rich sandstone (mostly SiO₂), possibly weakly metamorphosed quartzite
AI-generated identification · may be incorrectTan-brown, dull to slightly earthy luster, rounded by abrasion, and visibly granular or weathered. Quartz-rich material is typically Mohs 6–7, with no obvious cleavage; exact identification requires a fresh surface and hardness test.
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Physical properties
Tan-brown, dull to slightly earthy luster, rounded by abrasion, and visibly granular or weathered. Quartz-rich material is typically Mohs 6–7, with no obvious cleavage; exact identification requires a fresh surface and hardness test.
Formation & geological history
Most likely formed from compacted and cemented quartz sand, then rounded in a stream or shoreline environment; iron-oxide weathering produces the brown color. Its age cannot be determined from the photograph.
Uses & applications
Common sandstone is used as building stone, aggregate, and landscaping material; an ordinary pebble has little commercial or jewelry use.
Geological facts
The specimen’s rounded shape indicates transport after formation. A streak or scratch test can distinguish it from softer mudstone or shale.
Field identification & locations
Look for individual sand grains, layered bedding, and whether a steel knife scratches it; quartz-rich rock resists scratching, while sandstone may crumble or shed grains. Common worldwide in sedimentary terrains and river gravels.
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