sedimentary
Chert (Flint)
Microcrystalline silica (SiO2)
AI-generated identification · may be incorrectHardness: 7; Color: Gray, tan, or brown with iron staining; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); SG: 2.65.
- Hardness
- 7
- Color
- Gray, tan, or brown with iron staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7; Color: Gray, tan, or brown with iron staining; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); SG: 2.65.
Formation & geological history
Forms through the precipitation of silica from groundwater filling pores in sedimentary rocks or through the accumulation of siliceous organic remains in marine environments.
Uses & applications
Historical use for stone tools/weapons due to conchoidal fracture; modern use in construction aggregate, road surfacing, and as a sparking agent (flint).
Geological facts
Chert was one of the most important materials for early humans because its sharp edges were ideal for making arrowheads and scrapers. It is resistant to chemical weathering.
Field identification & locations
Identify by its extreme hardness (scratches glass) and smooth, curved shell-like fracture surfaces. Often found as nodules within limestone or chalk beds.
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