
sedimentary
Chert
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 Mohs; Color: Tan, beige, brown; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Color
- Tan, beige, brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, beige, brown; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture).
Formation & geological history
Forms primarily as nodules or beds in sedimentary rocks through the accumulation of silica-rich organic remains or chemical precipitation. Found in various geological eras.
Uses & applications
Historically used for stone tools due to sharp edges; currently used in construction as road metal and in lapidary work for tumbled stones and cabochons.
Geological facts
Flint is a dark variety of chert. It has been used since the Stone Age for making arrowheads and spear points because of the way it fractures into sharp edges.
Field identification & locations
Identified by its waxy appearance, extreme hardness (scratches glass), and distinctive shell-like (conchoidal) fracture pattern. Common in limestone deposits.
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Sandstone or Siltstone
Arenite (if sandstone)
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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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