
sedimentary
Chert
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 Mohs; Color: Tan, brown, or grayish; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
- Hardness
- 6
- Color
- Tan, brown, or grayish
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, brown, or grayish; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
Formation & geological history
Formed via the accumulation of siliceous remains of organisms or precipitation from silica-rich fluids within sedimentary basins; often found as nodules in limestone or chalk beds.
Uses & applications
Historically used for stone tools (arrowheads); currently used in road construction, as an abrasive, and occasionally for lapidary work.
Geological facts
Chert is essentially the same mineral as flint, but the name flint is usually reserved for dark varieties found in chalk. It is highly resistant to chemical weathering.
Field identification & locations
Identified by its extreme hardness (scratches glass) and its smooth, shell-like (conchoidal) fracture pattern. Commonly found in riverbeds and gravel pits.
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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
Argillaceous sedimentary rock
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Sandstone
Arenite (primarily SiO2)
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