
sedimentary
Chert (Jasper/Flint variant)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 7 (Mohs scale); Color: Tan, brown, and yellowish-brown; Luster: Waxy to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Tan, brown, and yellowish-brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Tan, brown, and yellowish-brown; Luster: Waxy to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or through the chemical precipitation of silica in groundwater. This specimen appears to be a weathered nodule, potentially from Paleozoic to Mesozoic era deposits.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; modernly used in road surfacing, decorative landscaping, and occasionally lapidary work if highly colorful.
Geological facts
Chert is so durable that it often survives as 'river gravel' long after the surrounding limestone or chalk has eroded away. Iron oxide impurities are what give this specific piece its yellowish-brown 'butterscotch' hue.
Field identification & locations
Identify in the field by its conchoidal (shell-like) fracture patterns and ability to scratch glass. It often has a smooth, waxy texture and often occurs as rounded nodules in stream beds or embedded in limestone.
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