
sedimentary
Chert (Flint)
Microcrystalline Quartz (SiO2)
Hardness: 7 Mohs scale. Color: Brown, tan, and gray with waxy luster. Conchoidal fracture (breaks like glass with curved edges). Cryptocrystalline structure. Specific gravity: 2.65.
- Hardness
- 7 Mohs scale
- Color
- Brown, tan, and gray with waxy luster
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Physical properties
Hardness: 7 Mohs scale. Color: Brown, tan, and gray with waxy luster. Conchoidal fracture (breaks like glass with curved edges). Cryptocrystalline structure. Specific gravity: 2.65.
Formation & geological history
Formed in marine environments through the precipitation of silica or the accumulation of silica-rich microfossils like radiolaria. Often found as nodules within limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads). Today used in landscaping, as a flint for fire-starting, and occasionally as a minor abrasive or for decorative gravel.
Geological facts
Flint is a variety of chert that occurs in chalk or marly limestone. It was the most important raw material for toolmaking throughout the Stone Age due to its predictable breaking pattern and sharp edges.
Field identification & locations
Identify in the field by its smooth, waxy surface and the presence of sharp, curved edges where it has chipped. It will easily scratch glass and will not react to acid. Commonly found in riverbeds and limestone outcrops.
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