
sedimentary
Chert (Jasper/Basalt River Pebble)
Silicon Dioxide (SiO2) or Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Dark grey, brown, olive-green; Luster: Waxy to dull; Crystal structure: Microcrystalline (hidden crystals); Cleavage: None (conchoidal fracture); Opaque to translucent edges.
- Hardness
- 6
- Color
- Dark grey, brown, olive-green
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Dark grey, brown, olive-green; Luster: Waxy to dull; Crystal structure: Microcrystalline (hidden crystals); Cleavage: None (conchoidal fracture); Opaque to translucent edges.
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in marine or river environments. This specific specimen appears to be water-worn, smoothed by fluvial (river) transport over thousands of years.
Uses & applications
Used historically for flint-knapping tools and weapons. Current uses include landscaping, road aggregate, and as a collector's specimen for tumbled stones.
Geological facts
Chert is a incredibly durable stone that resists weathering. Because of its hardness and ability to fracture into sharp edges, it was one of the most important stones used by prehistoric humans to create arrowheads and scrapers.
Field identification & locations
Identify by its 'waxy' texture when wet and its inability to be scratched by a steel knife. It is commonly found in riverbeds, glacial tills, and coastal beaches. Look for a smooth, rounded shape and a dull sheen.
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