sedimentary

Chert (Chert Nodule in Limestone)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 (Mohs scale), Color: Dark brown to black with white/tan matrix, Luster: Waxy to dull, Crystal Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Identified May 11, 2026More sedimentary →

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Physical properties

Hardness: 7 (Mohs scale), Color: Dark brown to black with white/tan matrix, Luster: Waxy to dull, Crystal Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or chemical precipitation within carbonate sedimentary environments. These nodules often displace limestone as they grow.

Uses & applications

Historically used for making stone tools (arrowheads/scrapers) due to its sharp edges; currently used as construction aggregate or as decorative landscape stones.

Geological facts

Chert is so hard it can strike sparks from steel, which led to its extensive use in flintlock firearms. Dark varieties are often specifically referred to as flint.

Field identification & locations

Identify by its waxy luster, extreme hardness (it will scratch glass), and conchoidal (shell-like) fracture pattern. Commonly found embedded in limestone or chalk outcrops.