
sedimentary
Chert (Jasper/Flint variety)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, and dark grey mottling. Luster: Dull to waxy. Crystal Structure: Hexagonal (microscopic). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.7.
- Hardness
- 6
- Color
- Brown, tan, and dark grey mottling
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, and dark grey mottling. Luster: Dull to waxy. Crystal Structure: Hexagonal (microscopic). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.7.
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation from groundwater within sedimentary beds, typically in marine environments. Age ranges from Precambrian to Recent.
Uses & applications
Historically used for stone tools (arrowheads). Modernly used in jewelry (lapidary), as a road aggregate, and for landscaping.
Geological facts
Chert has a conchoidal fracture which creates sharp edges, making it the primary material for prehistoric tool making. It is often found as nodules inside limestone or chalk beds.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by a steel knife) and its smooth, shell-like fracture pattern. Common in riverbeds and limestone outcrops globally.
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