
sedimentary
Rounded sandstone pebble
Quartz-rich sandstone (primarily SiO₂), possibly arkosic sandstone
AI-generated identification · may be incorrectFine- to medium-grained, tan to reddish-brown, matte and granular; composed mainly of quartz with feldspar and iron-oxide cement. Hardness is typically 6–7 for grains but variable overall; no visible cleavage, porous texture, and moderate specific gravity around 2.2–2.7.
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Physical properties
Fine- to medium-grained, tan to reddish-brown, matte and granular; composed mainly of quartz with feldspar and iron-oxide cement. Hardness is typically 6–7 for grains but variable overall; no visible cleavage, porous texture, and moderate specific gravity around 2.2–2.7.
Formation & geological history
Lithified sand deposited in a river, beach, dune, or shallow-marine environment, then naturally rounded by abrasion during transport. Its exact geological age cannot be determined from the image and may range from recent lithification to hundreds of millions of years.
Uses & applications
Commonly used as aggregate, building stone, paving, landscaping material, and occasionally in decorative crafts; this ordinary pebble has little jewelry value.
Geological facts
The rounded shape indicates substantial transport or wave abrasion. Iron oxides produce the warm tan and rusty coloration, while weathering can accentuate surface pores.
Field identification & locations
Identify it by visible sand-sized grains, gritty texture, lack of interlocking crystals, and possible layering or iron staining; it should not fizz strongly in dilute hydrochloric acid. Sandstone pebbles are common in streambeds, beaches, deserts, and glacial deposits.
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