
sedimentary
Chert (and Flint variant)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, tan, or brown; Luster: Waxy to dull; Structure: Microcrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, or brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, or brown; Luster: Waxy to dull; Structure: Microcrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6
Formation & geological history
Formed through the accumulation of silica-rich biogenic material such as radiolarian or diatoms, or by chemical precipitation in groundwater replacing limestone/chalk. Found throughout Earth's history from Precambrian to modern times.
Uses & applications
Historically used for stone tools and starting fires (flint). Currently used in road surfacing, as an abrasive, and for decorative landscaping.
Geological facts
Chert was one of the first materials harvested by early humans to create arrowheads and scrapers due to its sharp edges when broken. 'Flint' is a dark variety of chert commonly found in chalk deposits.
Field identification & locations
Identify by its waxy appearance and shell-like (conchoidal) curves on broken faces. It will scratch glass easily. Commonly found as nodules or layers in limestone beds.
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