
sedimentary
Chert (specifically Gray/Tan Chert Node)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, tan, brownish-green; Luster: Waxy to dull; Crystal structure: Cryptocrystalline/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, brownish-green
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, brownish-green; Luster: Waxy to dull; Crystal structure: Cryptocrystalline/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like diatoms or radiolaria) or through chemical precipitation within limestone or chalk beds. This specimen appears water-worn, suggesting it was found in a river or alluvial deposit.
Uses & applications
Historically used for stone tools and arrowheads; currently used as construction aggregate, road base, and as decorative landscape stone. It is also collected as a lapidary material for tumbling.
Geological facts
Chert has been used by humans for millions of years to create sharp-edged tools due to its conchoidal fracture. Some types of chert, like flint, were vital for starting fires in early history.
Field identification & locations
Identify in the field by its smooth, waxy feel, hardness (it will scratch glass), and the way it breaks into curved, shell-like flakes. Found globally in sedimentary basins and riverbeds.
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