
sedimentary
Chert (Jasper/Flint variant)
Microcrystalline quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Grayish-brown to olive; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 6
- Color
- Grayish-brown to olive
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Grayish-brown to olive; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); 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 chemical precipitation in marine environments. These specimens are often hundreds of millions of years old, typically found in nodules within limestone or chalk beds.
Uses & applications
Historically used for stone tools (arrowheads/scrapers) due to its sharp edges when fractured. Modernly used in construction aggregate, road surfacing, and as a semi-precious gemstone when colorful (Jasper).
Geological facts
Chert was one of the most vital materials for early humans; its ability to produce a predictable conchoidal fracture allowed for the creation of sophisticated tools and weaponry.
Field identification & locations
Identify in the field by its hardness (will scratch glass), waxy texture, and shell-like (conchoidal) fracture patterns. Look for it in riverbeds or eroding out of sedimentary rock layers.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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