
sedimentary
Chert (Yellow Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Yellow (due to iron oxide inclusions), tan, or mustard; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65.
- Hardness
- 6
- Color
- Yellow (due to iron oxide inclusions), tan, or mustard
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Yellow (due to iron oxide inclusions), tan, or mustard; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65.
Formation & geological history
Formed through the accumulation of silica-rich fluids or the replacement of limestone. It typically forms in marine environments where silica-rich organic remains (like radiolaria or diatoms) recrystallize over millions of years.
Uses & applications
Historical use in stone tools (arrowheads, scrapers) due to its sharp edges; modern uses include lapidary work, jewelry (cabs), and as a decorative landscaping stone.
Geological facts
Yellow chert or jasper has been used by humans for over 100,000 years. Because of its extreme hardness and ability to hold a sharp edge, it was a primary material for prehistoric survival tools.
Field identification & locations
Identify in the field by its smooth, shell-like (conchoidal) fracture and its ability to scratch glass. Widely found in riverbeds, glacial tills, and within limestone outcrops. Collectors look for pieces with unique patterns or deep coloration.
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