sedimentary

Chert (specifically a flint nodule component)

Microcrystalline quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: typically gray, tan, or brown with a white weathered cortex; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none (conchoidal fracture); Specific gravity: 2.65

Hardness: 7 on Mohs scale
Color: typically gray, tan, or brown with a white weathered cortex
Luster: waxy to dull

Identified May 1, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine sedimentary environments. It often occurs as nodules in limestone or chalk beds.

Uses & applications

Historically used for making stone tools (arrowheads, scrapers) due to its sharp edges; used in modern times as road aggregate, in glass manufacturing, and as a decorative stone in landscaping.

Geological facts

Chert is so hard it can scratch steel. When struck against steel, it creates sparks, leading to its historical use in flintlock firearms and fire-starting kits.

Field identification & locations

Identify by its extreme hardness, conchoidal fracture (curved, glass-like breaks), and waxy texture. Commonly found in stream beds or within limestone outcrops. Collectors look for pieces with distinct colors or fossil inclusions.