sedimentary

Chert (Iron-stained)

Chert (Microcrystalline Quartz, SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: Brown, tan, and reddish-orange due to limonite/hematite staining; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6 – 2.7.

Hardness: 7 on Mohs scale
Luster: Waxy to dull

Identified April 23, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the accumulation of silica-rich microfossils (like radiolarians or diatoms) or chemical precipitation from hydrothermal fluids in marine environments. This specimen shows significant weathering and oxidation of iron minerals.

Uses & applications

Historically used for making stone tools (arrowheads/scrapers) because of its sharp conchoidal fracture. Modern uses include road surfacing, decorative landscaping, and occasionally as an abrasive.

Geological facts

Chert is so hard that it can scratch steel. It was one of the most vital materials for prehistoric humans globally. Iron-stained varieties specifically indicate the presence of nearby iron-rich groundwater or minerals.

Field identification & locations

Identify in the field by its hardness (it will scratch glass), its shell-like (conchoidal) fracture pattern, and its smooth, waxy texture on fresh breaks. Found worldwide, particularly in limestone and dolomite formations.