
sedimentary
Chert (Flint variety)
Chert (SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs); Color: Dark grey to black with brownish weathering; Luster: Dull to waxy; Crystal structure: Microcrystalline/cryptocrystalline (concealed); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 6
- Color
- Dark grey to black with brownish weathering
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5–7 (Mohs); Color: Dark grey to black with brownish weathering; Luster: Dull to waxy; Crystal structure: Microcrystalline/cryptocrystalline (concealed); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from the accumulation of siliceous remains of marine organisms (like radiolarians or diatoms) or secondary chemical precipitation in limestone/chalk beds. Can range from Precambrian to Holocene in age.
Uses & applications
Historically used for stone tools and fire-starting. Modern uses include aggregate in construction, road surfacing, and as a polishing media in rock tumblers.
Geological facts
Flint was the most important raw material for early humans to create sharp-edged tools. When struck against steel or pyrite, it produces sparks, making it essential for early firearms (flintlocks).
Field identification & locations
Identify by its waxy texture and characteristic conchoidal (shell-like) fracture edges which are very sharp. Look for it in chalk or limestone outcrops. It will scratch glass easily.
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