
sedimentary
Yellow Chert
Sedimentary cryptocrystalline quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Yellowish-tan to mustard (due to iron oxides/limonite); Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Yellowish-tan to mustard (due to iron oxides/limonite)
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Yellowish-tan to mustard (due to iron oxides/limonite); Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolaria) or chemical precipitation in marine environments. This specimen likely dates from the Paleozoic or Mesozoic eras.
Uses & applications
Historically used for stone tools/arrowheads due to its sharp edges when broken. Today used as road base, decorative landscaping gravel, and occasionally for lapidary tumbling.
Geological facts
Chert is so durable that it often survives as 'river rocks' long after the surrounding limestone or shale has eroded away. Yellow varieties are frequently called 'Jasper' if they are opaque and highly pigmented.
Field identification & locations
Identify by its waxy texture, extreme hardness (it will scratch glass), and conchoidal (shell-like) fracture patterns. Frequently found in stream beds or weathered out of carbonate rock formations.
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