
sedimentary
Weathered sandstone pebble
Quartz-rich sandstone, likely ferruginous sandstone
AI-generated identification · may be incorrectFine-grained, tan-brown, dull to slightly gritty surface; composed mainly of quartz with feldspar, clay, and iron-oxide cement. Typical hardness is about 6–7 for individual grains, but the rock is relatively friable; no visible crystals or cleavage.
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Physical properties
Fine-grained, tan-brown, dull to slightly gritty surface; composed mainly of quartz with feldspar, clay, and iron-oxide cement. Typical hardness is about 6–7 for individual grains, but the rock is relatively friable; no visible crystals or cleavage.
Formation & geological history
Formed when sand was deposited, compacted, and cemented, commonly in river, dune, or shallow-marine settings. Its exact geological age cannot be determined from the photograph; surface weathering has rounded and darkened the specimen.
Uses & applications
Used as building stone, paving, aggregate, and occasionally decorative stone; this small weathered piece has primarily educational or modest collecting value.
Geological facts
Iron oxides produce the rusty brown coloration, while differential weathering can create the tapered, pebble-like shape.
Field identification & locations
Identify it by its gritty texture, visible sand grains, earthy tan color, and tendency to scratch glass only if strongly quartz-rich. Common worldwide in sedimentary terrains, stream beds, deserts, and eroding sandstone outcrops.
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