
sedimentary
Chert (specifically Flint or Jasper variant)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Brown, tan, and dark translucent patches; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Brown, tan, and dark translucent patches
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Brown, tan, and dark translucent patches; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic or chemical deposits in sedimentary environments. Often found as nodules in limestone or chalk beds. This specimen appears to have water-worn or weathered cortex.
Uses & applications
Historically used for stone tools (knapping) and fire-starting. Currently used as an abrasive, in decorative landscaping, or as a semi-precious gemstone when polished.
Geological facts
Chert was one of the most important lithic materials for prehistoric humans due to its predictable conchoidal fracturing, which allows for the creation of razor-sharp edges.
Field identification & locations
Identify by its waxy luster, hardness (can scratch glass), and shell-like (conchoidal) fractures on broken surfaces. Commonly found in riverbeds, gravel pits, and eroding out of limestone outcrops.
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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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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Shale or Slaty Mudstone
Argillaceous sedimentary rock
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Sandstone
Arenite (primarily SiO2)
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