
sedimentary
Chert (Nodule)
Chert (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Tan, gray, or brown; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.6
- Hardness
- 7 on Mohs scale
- Color
- Tan, gray, or brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, gray, or brown; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.6
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation within limestone or chalk beds, often under marine conditions.
Uses & applications
Historically used for stone tools and weapons (flint-knapping); currently used in road construction, landscaping, and as a polishing abrasive.
Geological facts
Chert is extremely durable and can preserve microfossils. It has been used by humans for hundreds of thousands of years to create sharp-edged tools due to its predictable breaking pattern.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), smooth waxy feel, and curved 'clamshell' fracture patterns. Common in sedimentary basins worldwide.
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