
sedimentary
Chert (specifically Pink Chert or Jasperized Chert)
Silicon Dioxide (SiO2) - Cryptocrystalline Quartz
Hardness: 7 (Mohs scale); Color: Pink, tan, and grey with iron oxide staining; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6 – 2.7.
- Hardness
- 7 (Mohs scale)
- Color
- Pink, tan, and grey with iron oxide staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Pink, tan, and grey with iron oxide staining; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6 – 2.7.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolaria) or chemical precipitation from hydrothermal fluids in limestone or volcanic environments. Often dates from the Paleozoic to Mesozoic eras.
Uses & applications
Historically used for stone tools (arrowheads/scrapers) due to sharp edges; currently used for road aggregate, landscaping, flint-knapping enthusiasts, and occasionally lapidary cabochons.
Geological facts
Chert is so hard it can strike sparks against steel, which is why varieties like flint were essential for early firearms. It is chemically very stable and resistant to weathering.
Field identification & locations
Identify in the field by its distinct conchoidal (shell-like) fracture patterns and ability to scratch glass. Commonly found in nodular form within limestone beds or as rounded river cobbles in gravel deposits.
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