
sedimentary
Chert (Jasper variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Red-brown, tan, and earthy tones due to iron impurities; Luster: Dull to waxy; Structure: Microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65
- Hardness
- 6
- Color
- Red-brown, tan, and earthy tones due to iron impurities
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Red-brown, tan, and earthy tones due to iron impurities; Luster: Dull to waxy; Structure: Microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation from hydrothermal fluids in sedimentary environments. Common in marine limestone formations.
Uses & applications
Historically used for making stone tools and arrowheads; modernly used as decorative gravel, in lapidary work for jewelry, and as a polishing abrasive.
Geological facts
Chert has a conchoidal fracture which means it breaks like glass, producing sharp edges that were essential for prehistoric survival. Jasper is the name specifically given to opaque varieties of chert.
Field identification & locations
Identify by its hardness (it will scratch glass) and its smooth, shell-like fracture surfaces. Frequently found in riverbeds, glacial till, and within limestone outcrops.
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