
sedimentary
Weathered sandstone pebble
Quartz-rich sandstone, commonly arkosic or ferruginous sandstone
AI-generated identification · may be incorrectTypically Mohs 6–7 for quartz grains, with a sandy texture, brown to reddish coloration from iron oxides, dull to weakly glossy luster, and no visible cleavage. Rounded edges and small pits indicate abrasion and weathering; exact composition cannot be confirmed from the image alone.
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Physical properties
Typically Mohs 6–7 for quartz grains, with a sandy texture, brown to reddish coloration from iron oxides, dull to weakly glossy luster, and no visible cleavage. Rounded edges and small pits indicate abrasion and weathering; exact composition cannot be confirmed from the image alone.
Formation & geological history
Formed when sand-sized grains, mainly quartz with possible feldspar, were compacted and cemented in an ancient river, beach, dune, or shallow-marine environment. Its rounded shape likely developed through prolonged transport; age is indeterminate.
Uses & applications
Used as a landscaping, aggregate, and decorative stone; attractive polished pieces may be used in craftwork, but this specimen has little gem value.
Geological facts
The rusty color generally reflects hematite or limonite cement. Small cavities may represent weathered grains or softer inclusions removed during erosion.
Field identification & locations
Identify it by visible granular texture, earthy brown-red color, rounded waterworn form, and lack of strong cleavage or crystal faces. Common in streambeds, beaches, gravel deposits, and eroded sandstone terrains worldwide.
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