
sedimentary
Chert (Agatized Chert)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grayish-yellow to translucent tan; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Grayish-yellow to translucent tan
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Grayish-yellow to translucent tan; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains or by the precipitation of silica from groundwater within limestone or other sedimentary formations. This specimen appears to be an agatized or chalcedony-rich variety often found in ancient marine beds.
Uses & applications
Historically used for stone tools (knapping) due to its sharp conchoidal edges; currently used for lapidary work, jewelry, and as a decorative landscaping stone.
Geological facts
Chert was one of the most important minerals for early humans, used to create arrowheads, scrapers, and blades. Because it is harder than steel, it can produce sparks when struck against iron, making it useful for fire-starting.
Field identification & locations
Identify in the field by its waxy texture and shell-like (conchoidal) fractures. It will easily scratch glass and cannot be scratched by a steel knife. Commonly found in stream beds or weathering out of limestone cliffs.
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