
sedimentary
Chert (Tan/Grey variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Tan, grey, white, or cream; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Tan, grey, white, or cream
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, grey, white, or cream; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation from silica-rich fluids within limestone or chalk beds. This specimen is typically found in sedimentary strata ranging from the Precambrian to Cenozoic eras.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp edges. Modern uses include road surfacing, jewelry (when colorful, known as jasper), and as an abrasive.
Geological facts
Chert is so hard it can scratch steel and produce sparks when struck against iron, making it a primary component for 'flint and steel' fire-starting kits. The specimen shown shows a classic conchoidal (shell-like) fracture pattern.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), its waxy feel, and the way it breaks into sharp, curved edges. Commonly found in nodules or layers within limestone and dolomite formations worldwide.
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