
sedimentary
Chert (specifically var. Flint or Jasper-rich Breccia)
Microcrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale); Color: Gray, tan, and reddish-pink patches in this specimen; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Gray, tan, and reddish-pink patches in this specimen
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Gray, tan, and reddish-pink patches in this specimen; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the precipitation of silica from groundwater or as a biochemical sediment on the ocean floor, filling voids in limestone or replacing carbonates. This specific specimen appears brecciated, likely formed in a high-pressure fault zone or collapse structure.
Uses & applications
Historically used for stone tools and weapons due to sharp edges; currently used for road surfacing, grinding media in industry, and occasionally as semi-precious gemstones (jasper).
Geological facts
Chert is so hard it can strike sparks from steel, a property that led to its use in flintlock firearms. It is incredibly durable and can survive millions of years of erosion.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife) and its curved, glass-like 'conchoidal' fracture patterns. Common in limestone regions and creek beds.
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