
sedimentary
Chert / Jasper
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Luster: Waxy to dull; Color: Earthy tones including brown, grey, dark red, and tan; Cleavage: None (conchoidal to irregular fracture); Crystal structure: Trigonal (microcrystalline).
- Hardness
- 6
- Color
- Earthy tones including brown, grey, dark red, and tan
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Luster: Waxy to dull; Color: Earthy tones including brown, grey, dark red, and tan; Cleavage: None (conchoidal to irregular fracture); Crystal structure: Trigonal (microcrystalline).
Formation & geological history
Formed in marine or sedimentary environments through the precipitation of silica-rich fluids or accumulation of siliceous organisms like radiolarians and diatoms, subsequently compacted over geological time.
Uses & applications
Historically used by indigenous peoples for making sharp tools and arrowheads due to its conchoidal fracture. Today it is used as decorative stone, in landscaping, lapidary arts, and stone tumbling.
Geological facts
Chert and jasper are varieties of microcrystalline quartz. Jasper specifically refers to the opaque, iron-rich, colorful varieties, while chert often refers to duller or grey/brown varieties.
Field identification & locations
Identified in the field by its high hardness (cannot be scratched by steel), sharp edges when broken, waxy luster, and smooth conchoidal fracture surfaces. Commonly found along riverbeds, gravel bars, and sedimentary rock formations.
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