
sedimentary
Chert
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: tan, brown, or grayish; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none; Fracture: conchoidal (shell-like)
- Hardness
- 7 (Mohs scale), Color: tan, brown, or grayish
- Color
- tan, brown, or grayish
- Luster
- waxy to dull
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Physical properties
Hardness: 7 (Mohs scale), Color: tan, brown, or grayish; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none; Fracture: conchoidal (shell-like)
Formation & geological history
Formed by the accumulation of silica-rich microfossils or via chemical precipitation in marine or groundwater environments. Found as nodules in limestone or as distinct bedded deposits.
Uses & applications
Historically used for making sharp tools like arrowheads and scrapers. Today used for construction aggregate, road base, and decorative landscaping.
Geological facts
Chert is so hard it can strike sparks from steel. Flint is a well-known dark variety of chert. It is extremely chemically stable and resistant to weathering.
Field identification & locations
Identify by its extreme hardness (scratches glass), waxy luster, and conchoidal fracture which creates sharp, curved edges. Frequently found in gravel pits or areas with limestone bedrock.
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