
sedimentary
Weathered sandstone or arkose pebble
Quartz-rich siliciclastic sandstone; likely arkose if feldspar-rich
AI-generated identification · may be incorrectHardness about 6–7 for quartz grains; pale pink, tan, and gray, with a dull earthy luster and visibly granular texture. No obvious cleavage; rounded, weathered clast with iron-oxide staining and possible thin cemented layers.
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Physical properties
Hardness about 6–7 for quartz grains; pale pink, tan, and gray, with a dull earthy luster and visibly granular texture. No obvious cleavage; rounded, weathered clast with iron-oxide staining and possible thin cemented layers.
Formation & geological history
Formed when sand-sized quartz and feldspar grains were deposited, compacted, and cemented, commonly in river, alluvial, or desert settings. Its precise geological age cannot be determined from the photograph; surface weathering produced the rounded exterior.
Uses & applications
Primarily a natural gravel or collectible specimen; sandstone is widely used as building stone, paving, aggregate, and occasionally dimension stone. This ordinary pebble has little commercial or jewelry value.
Geological facts
The pink coloration commonly reflects potassium feldspar or iron-oxide coatings, while the darker edge may be a more strongly cemented or finer-grained layer. The smooth shape indicates transport or prolonged weathering.
Field identification & locations
Look for sand-sized grains, layered or massive bedding, and a gritty texture; a hand lens can distinguish quartz from pink feldspar. Common in stream gravels and eroding sandstone terrains worldwide.
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