
sedimentary
Chert (Flint)
Microcrystalline Quartz (SiO2)
Hardness: 7 on the Mohs scale; Color: Grey, white, or tan with a waxy or dull luster; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Grey, white, or tan with a waxy or dull luster
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Physical properties
Hardness: 7 on the Mohs scale; Color: Grey, white, or tan with a waxy or dull luster; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed by the accumulation of siliceous remains of microscopic organisms like diatoms or radiolarians, or through chemical precipitation of silica from groundwater in limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads, knives) due to its sharp edges; used today as road surfacing material and for fire-starting in survival kits.
Geological facts
Chert has been used by humans for over 2 million years. When struck against steel, it produces sparks used to ignite gunpowder or tinder.
Field identification & locations
Identify by its characteristic shell-like (conchoidal) fracture pattern and its ability to scratch glass. Commonly found in nodular or bedded form within limestone outcrops.
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Cone-in-cone structure (Limestone)
Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Shale or Slaty Mudstone
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Sandstone
Arenite (primarily SiO2)
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