sedimentary
Chert Pebble
Microcrystalline silica (SiO2)
Hardness: 6.5-7 on Mohs scale. Color: Grey or brownish-grey. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Color
- Grey or brownish-grey
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Grey or brownish-grey. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture).
Formation & geological history
Formed via the accumulation of siliceous remains of marine organisms or through chemical precipitation in sedimentary basins over millions of years. This specific specimen appears water-worn into a pebble shape.
Uses & applications
Historically used for stone tools and fire-starting. Currently used as road aggregate, in landscaping, or as a tumble-polishing specimen for beginners.
Geological facts
Chert is composed of the same chemical material as quartz but has a much finer grain size. It was a primary material for prehistoric arrowheads due to its sharp conchoidal fracture.
Field identification & locations
Identified by its extreme hardness (scratches glass), waxy appearance, and smooth, rounded surface indicating fluvial or coastal erosion. Commonly found in riverbeds and glacial tills.
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