Rock Identifier
Tumbled reddish-brown pebble, likely iron-stained quartzite or sandstone (Probable quartzite (mostly SiO₂), though sandstone or chert is also possible from the photograph) — metamorphic
metamorphic

Tumbled reddish-brown pebble, likely iron-stained quartzite or sandstone

Probable quartzite (mostly SiO₂), though sandstone or chert is also possible from the photograph

AI-generated identification · may be incorrect

Hardness likely Mohs 6.5–7 for quartzite; opaque salmon-brown, fine-grained, smooth rounded surface, and dull to slightly waxy luster. No visible cleavage or distinct crystals; iron-oxide staining likely causes the color.

Identified More metamorphic
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Physical properties

Hardness likely Mohs 6.5–7 for quartzite; opaque salmon-brown, fine-grained, smooth rounded surface, and dull to slightly waxy luster. No visible cleavage or distinct crystals; iron-oxide staining likely causes the color.

Formation & geological history

If quartzite, it formed when quartz-rich sandstone was compressed and recrystallized during metamorphism, commonly hundreds of millions to billions of years ago. Its rounded shape indicates stream, beach, or deliberate tumbling abrasion.

Uses & applications

Suitable as a decorative pebble, landscaping stone, craft material, or low-cost lapidary specimen; generally little jewelry value unless it has attractive patterns or unusual provenance.

Geological facts

Quartzite commonly resists scratching and weathering better than sandstone. The image alone cannot reliably distinguish quartzite from iron-rich sandstone, chert, or another siliciclastic pebble.

Field identification & locations

Test with a steel knife: quartzite should resist scratching; a glass-scratch test is more diagnostic but may damage the surface. Common worldwide in river gravels, beaches, and glacial deposits.