
sedimentary
Yellow Chert (Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Opaque yellow to mustard brown; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
- Hardness
- 6
- Color
- Opaque yellow to mustard brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Opaque yellow to mustard brown; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine environments. The yellow color is typically caused by iron oxide inclusions (goethite). Age varies widely from Precambrian to Cenozoic.
Uses & applications
Used as lapidary material for jewelry (cabochons), ornamental carvings, and historically used for stone tools and arrowheads due to its sharp edges when fractured.
Geological facts
Chert is so durable that it often survives long after the surrounding rock has weathered away; it was one of the first minerals used by early humans for fire-starting and weaponry.
Field identification & locations
Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and the fact that it cannot be scratched by a steel knife. Common in riverbeds, glacial till, and embedded in limestone/dolomite formations.
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