
sedimentary
Chert (Brown variety / Common Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Brown, tan, or earthy yellow; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Brown, tan, or earthy yellow
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Brown, tan, or earthy yellow; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or the chemical precipitation of silica in marine environments. These specimens often originate in limestone or chalk beds as nodules and can range from ancient Precambrian to recent geological ages.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; modern uses include landscaping, road aggregate, jewelry (when polished as jasper), and as a gemstone for lapidary hobbyists.
Geological facts
Because it is extremely hard and chemically stable, chert often survives erosion that destroys surrounding rock. It was one of the most important minerals for early humans to create survival tools like arrowheads and scrapers.
Field identification & locations
Identify in the field by its smooth, waxy surface and its ability to scratch glass. Look for curved, shell-like (conchoidal) fractures on broken edges. It is commonly found in riverbeds or within sedimentary rock outcrops globally.
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