sedimentary

Chert (with Desert Varnish/Iron Stain)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 (Mohs scale), Color: tan to dark brown/black surface, Luster: waxy to dull, Structure: microcrystalline quartz, Cleavage: none (conchoidal fracture), Specific Gravity: 2.65

Identified April 12, 2026More sedimentary →

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Physical properties

Hardness: 7 (Mohs scale), Color: tan to dark brown/black surface, Luster: waxy to dull, Structure: microcrystalline quartz, Cleavage: none (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed from the accumulation of silica-rich microfossils (like radiolaria or diatoms) or chemical precipitation from groundwater. This specimen shows a dark 'desert varnish' or iron-rich oxidation layer likely from long-term exposure to arid environments.

Uses & applications

Historically used for making stone tools (arrowheads and scrapers) due to its conchoidal fracture. Today used in construction aggregate and as a collector's specimen.

Geological facts

Chert is remarkably durable and resistant to chemical weathering. When struck against steel, it can produce sparks, which made certain varieties (Flint) vital for early firearms and fire-starting.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by a steel nail) and the shell-like (conchoidal) curves where it has chipped. Commonly found in limestone beds or as nodules in desert pavements.