
sedimentary
Chert (Flint variety)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or white; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, brown, or white
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or white; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or the chemical replacement of limestone/dolomite by silica-rich groundwater. Often found as nodules or lenses within carbonate rock layers.
Uses & applications
Historically used for stone tools (arrowheads, knives) and strike-a-lights. Modernly used as a decorative stone, road aggregate, and for making high-quality ceramics or as a grinding medium.
Geological facts
Because it fractures conchoidally to produce razor-sharp edges, it was the most important material for early human technology. Flint (a dark variety of chert) was essential for spark-ignition systems in early firearms.
Field identification & locations
Identify in the field by its smooth, waxy surface and its ability to scratch glass. Look for the distinct 'shell-like' curved fracture patterns. It is extremely common in areas with limestone bedrock globally.
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