Rock Identifier
Rounded quartz-rich pebble (Likely quartzite or quartz-bearing sandstone; composition mainly SiO₂ with possible feldspar and iron-oxide impurities) — sedimentary
sedimentary

Rounded quartz-rich pebble

Likely quartzite or quartz-bearing sandstone; composition mainly SiO₂ with possible feldspar and iron-oxide impurities

AI-generated identification · may be incorrect

Gray-brown, subrounded to rounded, fine-grained and dull to subtly sparkly; quartz hardness 7, no obvious cleavage, conchoidal to uneven fracture, and typical specific gravity around 2.6–2.7. The surface appears naturally weathered rather than crystalline or gem-quality.

Identified More sedimentary
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Physical properties

Gray-brown, subrounded to rounded, fine-grained and dull to subtly sparkly; quartz hardness 7, no obvious cleavage, conchoidal to uneven fracture, and typical specific gravity around 2.6–2.7. The surface appears naturally weathered rather than crystalline or gem-quality.

Formation & geological history

Probably formed as a sedimentary pebble through river or beach abrasion; if quartzite, its original sandstone was metamorphosed and recrystallized. Exact geological age and provenance cannot be determined from the photograph.

Uses & applications

Primarily a natural pebble, specimen, or decorative material; not generally suitable for jewelry unless polished and attractive. Quartz-rich varieties may be used as aggregate or dimension stone.

Geological facts

The rounded shape records prolonged transport or wave action, while the pale patches may reflect quartz-rich areas, weathering, or adhered sediment.

Field identification & locations

Look for a uniformly hard, quartz-rich texture that scratches glass and does not fizz in dilute hydrochloric acid; a hand lens can distinguish interlocking quartz grains from sand-sized grains in sandstone. Common in streambeds, beaches, and glacial deposits worldwide.