
sedimentary
Chert (Jasper variety)
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Brown to reddish-orange (due to iron inclusions); Luster: Dull to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 6
- Color
- Brown to reddish-orange (due to iron inclusions)
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Brown to reddish-orange (due to iron inclusions); Luster: Dull to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation in sedimentary environments. Common in marine settings and as nodules in limestone. This sample shows signs of alluvial weathering.
Uses & applications
Historically used for tools and flintknapping. In modern times, used for lapidary jewelry, garden landscaping, and as a semi-precious gemstone when polished.
Geological facts
Chert is so durable that it was once the primary material for prehistoric arrowheads and spear tips because it breaks into sharp, glass-like edges. The brown variety is often influenced by limonite or goethite.
Field identification & locations
Identify by its hardness (it will scratch glass) and its curved, shell-like (conchoidal) fracture pattern. It feels smoother than sandstone and is found in riverbeds and coastal regions worldwide.
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