sedimentary

Chert (with Quartz veins)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5-7 (Mohs scale); Color: Brown, tan, or grey with white veins; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7

Hardness: 6
Color: Brown, tan, or grey with white veins
Luster: Waxy to dull

Identified April 23, 2026More sedimentary →

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Brown, tan, or grey with white veins; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolaria) or chemical precipitation in marine environments. The white veins are typically secondary quartz or calcite that filled fractures in the rock at a later stage.

Uses & applications

Historically used for stone tools (arrowheads/scrapers) due to its sharp edges; used today as a decorative landscaping stone, in construction aggregate, or as a lapidary material for tumbling.

Geological facts

Chert is so durable that it often survives as rounded pebbles in stream beds long after regular limestone has eroded away. It was one of the primary 'high-tech' materials of the Stone Age due to its predictable fracturing patterns.

Field identification & locations

Identify by its waxy texture and shell-like (conchoidal) fractures. It will easily scratch glass. Commonly found in riverbeds, gravel pits, and as nodules within limestone formations.