
sedimentary
Chert / River Pebble
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale. Luster: Dull, waxy, or earthy. Color: Brownish-gray with tan or reddish weathering crust/banding. Structure: Cryptocrystalline, smooth water-worn texture with conchoidal fracture potential.
- Hardness
- 6
- Color
- Brownish-gray with tan or reddish weathering crust/banding
- Luster
- Dull, waxy, or earthy
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Luster: Dull, waxy, or earthy. Color: Brownish-gray with tan or reddish weathering crust/banding. Structure: Cryptocrystalline, smooth water-worn texture with conchoidal fracture potential.
Formation & geological history
Formed through the accumulation and recrystallization of silica-rich organic remains or chemical precipitation in sedimentary environments, followed by natural erosion, tumbling, and smoothing in a river bed or beach setting.
Uses & applications
Commonly used as aggregate, landscaping gravel, river rock filler, and historically for stone tools such as arrowheads due to its sharp conchoidal fracture.
Geological facts
River pebbles made of chert or fine-grained quartzite are extremely durable and can travel hundreds of miles down river systems, becoming rounded and polished by natural water action over thousands to millions of years.
Field identification & locations
Identified by its extreme smoothness, rounded wedge shape, hard surface that resists scratching with steel, and distinct brownish color zones from iron-rich weathering. Widely found along riverbanks, lake shores, and glacial deposits globally.
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