
sedimentary
Chert (often called Flint or Jasper)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: typically tan, brown, or gray with reddish oxidation; Luster: waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: none (fractures conchoidally); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- typically tan, brown, or gray with reddish oxidation
- Luster
- waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: typically tan, brown, or gray with reddish oxidation; Luster: waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: none (fractures conchoidally); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or by chemical precipitation in limestone or chalk beds. Often Cretaceous to Paleozoic in age.
Uses & applications
Used historically for stone tools and arrowheads; currently used as road aggregate, in glassmaking (if high purity), and polished as semi-precious gemstones for jewelry (jasper variants).
Geological facts
Because it breaks with a conchoidal fracture (smooth, curved surfaces), it can produce edges sharper than a surgical scalpel. It was one of the most vital survival resources for prehistoric humans.
Field identification & locations
Identify in the field by its extreme hardness (cannot be scratched by a steel knife) and waxy texture. To test, look for rounded, shell-like fracture marks. Common in limestone exposures and riverbeds worldwide.
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