Rock Identifier
Chert / Flint (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert / Flint

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Gray to dull brown; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
7 (Mohs scale)
Color
Gray to dull brown
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 7 (Mohs scale); Color: Gray to dull brown; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed as nodules or layered deposits in sedimentary rocks (typically limestone or chalk) through the accumulation of silica-rich organic remains or chemical precipitation from groundwater.

Uses & applications

Historically used for stone tools and starting fires; currently used as construction aggregate, road base, and occasionally in lapidary work.

Geological facts

Flint is a variety of chert that was essential to prehistoric humans for making arrowheads and axes due to its ability to break into sharp edges through conchoidal fracturing.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by steel) and smooth, shell-like (conchoidal) breaks. Found globally in sedimentary basins.