
sedimentary
Chert (specifically Flint or Jasper variant)
Microcrystalline quartz (SiO2)
Hardness: 6.5–7 on Mohs scale. Color: Dark brown to black with reddish-brown edges. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (exhibits conchoidal fracture). Specific Gravity: 2.6–2.7.
- Hardness
- 6
- Color
- Dark brown to black with reddish-brown edges
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5–7 on Mohs scale. Color: Dark brown to black with reddish-brown edges. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (exhibits conchoidal fracture). Specific Gravity: 2.6–2.7.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or the chemical precipitation of silica in sedimentary basins. This specimen appears water-worn, suggesting a secondary transport history in a river or coastal environment.
Uses & applications
Historically used for making stone tools (knapping) due to its sharp edges. Currently used in construction aggregate, as a fire-starter (flint), and lower-quality pieces are used for landscaping or as aquarium stones.
Geological facts
Chert was one of the most vital materials for prehistoric humans; its ability to break into consistent, razor-sharp edges allowed for the creation of spears, arrowheads, and knives long before the Bronze Age.
Field identification & locations
Identify in the field by its smooth, waxy feel and the shell-like (conchoidal) curves where it has broken. Look for it in limestone or chalk deposits. It will easily scratch glass and strike sparks against steel.
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