
sedimentary
Chert (Jasper)
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Red, brown, and ochre due to iron oxides; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Color
- Red, brown, and ochre due to iron oxides
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Red, brown, and ochre due to iron oxides; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed through the accumulation of silica-rich fluids or organic remains (like radiolarians) in sedimentary environments. The red/brown coloration suggests high iron content (hematite/goethite staining).
Uses & applications
Historically used for stone tools due to its sharp edges. Modernly used for lapidary work, landscaping, and as a semi-precious gemstone in jewelry.
Geological facts
Chert is so durable that it can survive millions of years of erosion. When struck against steel, it can produce sparks, leading to its historical use in flintlock firearms.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by a steel knife) and its smooth, shell-like (conchoidal) fracture patterns. Frequently found in riverbeds or as nodules within limestone layers.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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