
sedimentary
Chert Nodule
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Brown, grey, or black with a weathered exterior; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Brown, grey, or black with a weathered exterior
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Brown, grey, or black with a weathered exterior; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed by the precipitation of silica from groundwater or the accumulation of silica-rich microfossils in limestone or chalk beds. Commonly found in sedimentary basins worldwide.
Uses & applications
Historically used for stone tools (flintknapping); currently used as an abrasive, decorative stone in landscaping, or for gravel construction.
Geological facts
Chert is one of the most durable sedimentary rocks and was the primary material for prehistoric arrowheads and spear points due to its sharp edges when broken.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by a steel nail) and characteristic conchoidal fracture patterns similar to thick glass. Look for rounded or irregular lumps in limestone outcrops.
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