Rock Identifier
Rounded river cobble, likely quartz-rich sandstone or quartzite (Indeterminate quartz-rich clastic rock; probable sandstone (SiO₂-rich)) — sedimentary
sedimentary

Rounded river cobble, likely quartz-rich sandstone or quartzite

Indeterminate quartz-rich clastic rock; probable sandstone (SiO₂-rich)

AI-generated identification · may be incorrect

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).

Identified More sedimentary
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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.