
sedimentary
Chert (Commonly known as Jasper or Flint)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Yellow-brown, tan, and grey; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 6
- Color
- Yellow-brown, tan, and grey
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Yellow-brown, tan, and grey; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed via the accumulation of silica-rich microfossils (like radiolaria or diatoms) or chemical precipitation of silica in marine or groundwater environments. It typically forms nodules in limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads). Modern uses include construction aggregate, road surfacing, and as a semi-precious gemstone in jewelry when it displays attractive colors (Jasper).
Geological facts
Chert has been used by humans for over 2 million years because its conchoidal fracture produces extremely sharp edges. It is chemically identical to quartz but has a different internal structure.
Field identification & locations
Identify by its hardness (it will scratch glass), its waxy feel, and its shell-like (conchoidal) fracture pattern. Commonly found in riverbeds, glacial tills, and sedimentary rock outcrops.
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