
sedimentary
Chert (White Chert / Flint)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Pure white to off-white; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Pure white to off-white
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Pure white to off-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 radiolarians or sponge spicules) or by the replacement of carbonate minerals in limestone/chalk. Found in sedimentary layers of various ages.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp edges; used today as road surfacing, in ceramics, and as a component in concrete.
Geological facts
Because it breaks with a conchoidal fracture (smooth, curved surfaces), it was the primary material for prehistoric humans to craft weapons. It is chemically very stable and resistant to weathering.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by steel) and curved, glass-like fracture surfaces. Often found as nodules within limestone or chalk beds.
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