
sedimentary
Chert (Iron-stained variant)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Tan, cream, with reddish-orange iron staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Tan, cream, with reddish-orange iron staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, cream, with reddish-orange iron staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine or groundwater environments. Can range from Precambrian to Cenozoic in age.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; modernly used as road aggregate, in landscaping, and as a low-cost lapidary material for tumbling.
Geological facts
Because of its hardness and conchoidal fracture, it was the primary material used by prehistoric humans to create arrowheads, scrapers, and knives. It is also known as 'flint' when found in chalk or marl.
Field identification & locations
Identify in the field by its hardness (it scratches glass easily) and its shell-like (conchoidal) breakage patterns. Often found as nodules in limestone or as distinct bedded layers in riverbeds.
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