
sedimentary
Chert (Yellow Jasper/Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7.0 (Mohs scale); Color: Yellow to tan with iron staining; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7
- Color
- Yellow to tan with iron staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7.0 (Mohs scale); Color: Yellow to tan with iron staining; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed as a sedimentary rock through the accumulation of silica-rich microfossils or chemical precipitation within limestone or dolostone layers. This water-worn specimen likely originated from Paleozoic or Mesozoic strata and was tumbled in a riverbed.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges. Currently used as an abrasive, in decorative landscaping, or as a lapidary material for tumbling and cabochons.
Geological facts
Chert is so durable that it often survives long after its original host rock has eroded away. Yellow varieties are frequently called 'Yellow Jasper' when opaque and are colored by goethite or limonite inclusions.
Field identification & locations
Identify by its waxy feel, hardness (will scratch glass), and lack of visible grains. Common in river gravels and outcrops throughout North America. Collectors look for smooth, colorful nodules free of internal fractures.
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