
sedimentary
Chert (Chalcedony)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Tan, brown, grey, or yellowish; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
- Hardness
- 6
- Color
- Tan, brown, grey, or yellowish
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Tan, brown, grey, or yellowish; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
Formation & geological history
Formed as a chemical precipitate or biochemical deposit, typically from the accumulation of siliceous oozes at the bottom of the ocean or through the replacement of limestone by silica-rich fluids.
Uses & applications
Historically used for stone tools (arrowheads); currently used as a semi-precious stone in jewelry, as high-quality aggregate in construction, and for precision laboratory grinding equipment.
Geological facts
Chert is so hard it can strike sparks against steel. Flint is a common variety of dark chert. It has been used by humans for hundreds of thousands of years to create sharp-edged tools and weapons.
Field identification & locations
Identify in the field by its waxy appearance, extreme hardness (it will scratch glass), and its shell-like (conchoidal) fracture pattern. It is common in limestone formations and riverbeds globally.
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Cone-in-cone structure (Limestone)
Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Clastic Sedimentary Rock Grain (SiO2 dominated)
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Shale or Slaty Mudstone
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Arenite (primarily SiO2)
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