
sedimentary
Water-worn gray sandstone or quartzite pebble
Quartz-rich sandstone (possibly weakly metamorphosed quartzite), chiefly SiO₂
AI-generated identification · may be incorrectHardness approximately 6–7 Mohs; gray, tan, and iron-oxide brown coloration; dull to subtly sugary luster; rounded by abrasion. Quartz grains are visible, with no obvious cleavage and likely moderate-to-high density.
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Physical properties
Hardness approximately 6–7 Mohs; gray, tan, and iron-oxide brown coloration; dull to subtly sugary luster; rounded by abrasion. Quartz grains are visible, with no obvious cleavage and likely moderate-to-high density.
Formation & geological history
Most likely lithified quartz-rich sand later compacted and cemented, then rounded in a river or beach; if quartzite, it underwent later metamorphism. Exact geological age cannot be determined from the photograph.
Uses & applications
Commonly used as landscaping stone, aggregate, paving material, and decorative stone; attractive polished pieces may be sold as low-cost specimens.
Geological facts
The smooth oval shape is environmental rather than crystal-controlled, produced by prolonged transport and abrasion. Rust-colored patches indicate oxidation of iron-bearing minerals or cement.
Field identification & locations
Identify by gritty granular texture, abundant quartz, lack of strong foliation, and inability to scratch it with a steel nail if quartzite-like; acid reaction should be absent. Common worldwide in streambeds, beaches, and glacial deposits.
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