
sedimentary
Chert (Jasper)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Reddish-brown, tan, or earth tones; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
- Hardness
- 6
- Color
- Reddish-brown, tan, or earth tones
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown, tan, or earth tones; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
Formation & geological history
Formed from the accumulation of silica-rich organic remains or chemical precipitation within sedimentary rock environments. Often found as nodules or beds in limestone or dolostone. Geological age ranges widely throughout the Phanerozoic eon.
Uses & applications
Historically used for stone tools/arrowheads due to its sharp conchoidal fracture. Currently used in landscaping, as aquarium gravel, and occasionally tumbled for jewelry or pocket stones.
Geological facts
Because it is composed of microcrystalline quartz, it is very resistant to physical and chemical weathering, meaning it often remains intact long after its host rock has eroded away. Jasper is the name specifically given to colorful, opaque varieties of chert.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), waxy appearance, and smooth, curved (conchoidal) breaks. Typically found in riverbeds, glacial till, or eroding out of sedimentary outcrops.
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