
sedimentary
Chert (potentially Jasper/Common Opal mixture)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Variable (browns, tans, purple-grey); Luster: Dull to waxy; Crystal Structure: Cryptocrystalline (non-visible); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Variable (browns, tans, purple-grey)
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Variable (browns, tans, purple-grey); Luster: Dull to waxy; Crystal Structure: Cryptocrystalline (non-visible); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Forms primarily through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from silica-rich fluids. Often found in seafloor deposits or as nodules in limestone/chalk.
Uses & applications
Historically used for stone tools (arrowheads). Currently used as an industrial abrasive, in road construction (aggregate), and as decorative landscaping stone. High-quality colorful pieces are used for lapidary work.
Geological facts
Because it breaks with a conchoidal fracture like glass, it creates extremely sharp edges; it was one of the most vital materials for prehistoric human survival.
Field identification & locations
Identify by its smooth, flint-like fracture and high hardness (it will scratch glass but cannot be scratched by a steel knife). Commonly found in sedimentary basins and riverbeds as rounded 'river rocks'.
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