
sedimentary
Flint / Chert
Silicon Dioxide (SiO2)
Hardness: 6.5-7 Mohs; Color: Grey, black, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 6
- Color
- Grey, black, or brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Grey, black, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed as nodules in sedimentary rocks like chalk and limestone through the replacement of calcium carbonate by silica-rich fluids. Often contains microscopic fossil remains.
Uses & applications
Historically used for stone tools and starting fires; currently used in grinding media, road construction, and as a decorative stone.
Geological facts
Flint was the primary material for the Stone Age technology due to its ability to break into sharp edges. It produces sparks when struck against steel.
Field identification & locations
Look for a glassy or waxy interior and sharp, shell-like (conchoidal) fractures when broken. Commonly found in coastal chalk cliffs or gravel deposits.
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