sedimentary

Chert (with Quartz Veining)

Microcrystalline silicon dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 (Mohs scale); Color: Dark grey to green-grey; Luster: Waxy to dull/earthy; Crystal Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness: 7 (Mohs scale)
Color: Dark grey to green-grey
Luster: Waxy to dull/earthy

Identified April 20, 2026More sedimentary →

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Physical properties

Hardness: 7 (Mohs scale); Color: Dark grey to green-grey; Luster: Waxy to dull/earthy; Crystal Structure: 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 from groundwater. This specimen shows secondary hydrothermal activity with quartz veining filling fractures.

Uses & applications

Historically used for stone tools (flintknapping). Today used as decorative stone, construction aggregate, and occasionally for folk medicine or in aquariums.

Geological facts

Chert is so hard it can scratch steel. When struck against steel, it can produce sparks, leading to its historical use as 'firestone'.

Field identification & locations

Identify in the field by its extreme hardness, smooth waxy texture on fresh surfaces, and tendency to break like glass (conchoidal fracture). Common in limestone or dolostone formations.