
sedimentary
Chert (Flint)
Chert (SiO2)
Hardness: 7.0 (Mohs); Color: Grey, brown, or white; Luster: Waxy to dull; Crystal structure: Microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
- Hardness
- 7
- Color
- Grey, brown, or white
- Luster
- Waxy to dull
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Physical properties
Hardness: 7.0 (Mohs); Color: Grey, brown, or white; Luster: Waxy to dull; Crystal structure: Microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
Formation & geological history
Formed by the precipitation of silica in sedimentary environments, often from the remains of siliceous organisms like diatoms or radiolarians, or through chemical replacement within limestone.
Uses & applications
Historically used for stone tools and fire-starting; currently used in construction aggregate, road surfacing, and as high-quality decorative river stones.
Geological facts
Chert has been used by humans for millions of years to create sharp-edged tools like arrowheads. When struck against steel, it produces sparks used to start fires.
Field identification & locations
Identify by its extreme hardness (scratches glass), waxy luster on fresh surfaces, and distinctive shell-like (conchoidal) fracture patterns. Frequently found in limestone beds.
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