
sedimentary
Chert (Jasper/Flint variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible iron oxide staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 7 on Mohs scale
- Color
- Tan, brown, and grey with possible iron oxide staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible iron oxide staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich microfossils (like radiolaria or diatoms) or by chemical precipitation in marine or groundwater environments. Often found as nodules in limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads/scrapers) due to conchoidal fracturing. Modern uses include road surfacing, decorative gravel, and lapidary work (polishing into cabochons).
Geological facts
Because it breaks with a very sharp edge, chert was one of the most important minerals for early human technological development. It is also sparks when struck against steel, making it vital for early fire-starting and flintlock firearms.
Field identification & locations
Identify by its waxy texture, extreme hardness (it will scratch glass), and the way it breaks into curved, shell-like (conchoidal) shards. Commonly found in creek beds or limestone outcrops.
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