
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 incorrectHardness 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.
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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.
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