
sedimentary
Chert (Flint)
Chert (Microcrystalline Quartz, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Gray, tan, and brown; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7. Highly durable and glass-like when broken.
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, and brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, and brown; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7. Highly durable and glass-like when broken.
Formation & geological history
Formed via the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation from silica-rich fluids within limestone or chalk beds. Often found as nodules or pebbles tumbled by water.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) and starting fires. Modernly used in road construction, gravel, and occasionally as lapidary material for jewelry.
Geological facts
Flint is a variety of chert that was essential to human survival for millennia due to its ability to produce sparks when struck against steel and its sharp edges when fractured.
Field identification & locations
Identify in the field by its smooth, waxy texture, conchoidal (shell-like) fracture patterns, and its ability to scratch glass. Commonly found in stream beds, beaches, and within sedimentary rock outcrops.
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