sedimentary

Chert (variously identified as Flint)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: Black, grey, white, and tan; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness: 7 on Mohs scale
Color: Black, grey, white, and tan
Luster: Waxy to vitreous

Identified April 18, 2026More sedimentary →

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Physical properties

Hardness: 7 on Mohs scale; Color: Black, grey, white, and tan; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation in marine environments. Often found as nodules within limestone or chalk beds.

Uses & applications

Historically used for stone tools and weapons (arrowheads). Modern uses include road construction aggregate, fire-starting strikers, and as a decorative stone for lapidary work.

Geological facts

Chert was one of the first materials used by early humans to create sharp tools due to its conchoidal fracture. It is extremely chemically stable and resistant to weathering, which is why it often appears as rounded river or beach pebbles.

Field identification & locations

Identify in the field by its extreme hardness (cannot be scratched by a steel knife) and its smooth, shell-like (conchoidal) fracture surfaces. Commonly found in riverbeds or coastal areas where softer surrounding rock has eroded away.