
sedimentary
Chert (Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Tan, brown, ochre; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
- Hardness
- 6
- Color
- Tan, brown, ochre
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Tan, brown, ochre; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation in marine or groundwater environments; often associated with limestone or replacement in sedimentary beds.
Uses & applications
Historically used for stone tools/arrowheads; currently used in landscaping, as a gemstone when colorful (Jasper), and as a structural aggregate in construction.
Geological facts
Chert was one of the most important minerals for early humans because its conchoidal fracture produces razor-sharp edges. It is chemically identical to quartz but has a different micro-structure.
Field identification & locations
Identify by its hardness (scratches glass), waxy luster, and shell-like (conchoidal) fracture pattern. Found globally in riverbeds, glacial tills, and sedimentary outcrops.
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