
sedimentary
Rounded river cobble, likely quartz-rich sandstone or quartzite
Indeterminate quartz-rich clastic rock; probable sandstone (SiO₂-rich)
AI-generated identification · may be incorrectPale gray, fine-grained, subrounded cobble with dull earthy luster and minor rusty iron-oxide staining. Likely hardness ~6–7 Mohs; no visible cleavage, weak granular texture, and moderate-to-high density (~2.5–2.7 g/cm³).
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Physical properties
Pale gray, fine-grained, subrounded cobble with dull earthy luster and minor rusty iron-oxide staining. Likely hardness ~6–7 Mohs; no visible cleavage, weak granular texture, and moderate-to-high density (~2.5–2.7 g/cm³).
Formation & geological history
Formed from compacted and cemented quartz-rich sediment, possibly later metamorphosed into quartzite, then rounded by stream or beach abrasion. Exact age and formation environment cannot be determined from the photograph.
Uses & applications
As an individual specimen it has little commercial value; similar material is used as aggregate, landscaping stone, road base, and occasionally decorative building stone.
Geological facts
The smooth oval shape reflects prolonged transport in moving water or wave action. Rust-colored patches commonly result from oxidation of trace iron-bearing minerals.
Field identification & locations
Test hardness against glass: scratching glass suggests quartzite or strongly cemented sandstone; a dilute hydrochloric-acid test should show no reaction. Common in river gravels, beaches, and glacial deposits.
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