
sedimentary
Weathered sandstone or iron-rich sedimentary cobble
Quartz-rich sandstone, possibly ferruginous sandstone
AI-generated identification · may be incorrectBrown to reddish-brown, dull earthy luster, visibly granular texture, and rounded weathered shape. Likely hardness about 6–7 due to quartz; no obvious cleavage or crystal faces, with moderate specific gravity around 2.3–2.7.
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Physical properties
Brown to reddish-brown, dull earthy luster, visibly granular texture, and rounded weathered shape. Likely hardness about 6–7 due to quartz; no obvious cleavage or crystal faces, with moderate specific gravity around 2.3–2.7.
Formation & geological history
Formed when sand-sized grains—mostly quartz, with iron-oxide cement—were compacted and lithified, then rounded by erosion and transport. Its precise geological age cannot be determined from the photograph.
Uses & applications
Common sandstone is used as building stone, paving, aggregate, and occasionally decorative material; this small cobble has little commercial value but may be a useful teaching or collection specimen.
Geological facts
The reddish-brown coloration typically comes from hematite or limonite coatings and cement. Surface rounding indicates transport by water, waves, or prolonged weathering.
Field identification & locations
Identify it by rubbing a fresh surface: visible sand grains and a gritty texture support sandstone; quartz-rich pieces resist scratching by a steel knife. Common in riverbeds, beaches, deserts, and sedimentary outcrops worldwide.
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