
sedimentary
Chert (Jasper variety)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Reddish-pink, tan, or brown due to iron inclusions; Luster: Dull to waxy; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.8
- Hardness
- 6
- Color
- Reddish-pink, tan, or brown due to iron inclusions
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Reddish-pink, tan, or brown due to iron inclusions; Luster: Dull to waxy; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.8
Formation & geological history
Formed through the accumulation of silica-rich microfossils (like radiolaria or diatoms) or chemical precipitation from hydrothermal fluids in sedimentary environments. Common in marine limestone formations.
Uses & applications
Historically used for stone tools/arrowheads due to its sharp fracture edges. Today used in construction aggregate, landscaping, lapidary work (polishing), and as a gemstone for jewelry (beads/cabochons).
Geological facts
Chert and its varieties like Jasper have been used since the Stone Age. When struck against steel, it can produce sparks, making it a primitive tool for fire-starting.
Field identification & locations
Identify in the field by its characteristic smooth, curved (conchoidal) fracture surfaces and its ability to scratch glass. Commonly found in river beds, gravel pits, and eroding out of sedimentary outcrops.
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