
sedimentary
Chert Pebble
Microcrystalline or Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible banding; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Tan, brown, and grey with possible banding
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, brown, and grey with possible banding; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine or groundwater environments. This specimen appears water-worn from a stream or alluvial deposit.
Uses & applications
Historically used for stone tools and weapons due to sharp fractures. Currently used in road construction (aggregate), decorative landscaping, and occasionally as minor gemstones (gem silica).
Geological facts
Chert is so hard it can create sparks when struck against steel, a property that led to its use in flintlock firearms. It is chemically identical to quartz and amethyst but has much smaller crystal units.
Field identification & locations
Identify in the field by its smooth, waxy texture and curved (conchoidal) breaks that resemble glass. Common in riverbeds and limestone outcrops. Collectors look for unique banding or fossil inclusions.
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