sedimentary

Chert (specifically Flint or Jasper variant)

Microcrystalline or Cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: Brownish-tan with a pinkish band; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness: 7 on Mohs scale
Color: Brownish-tan with a pinkish band
Luster: Waxy to dull

Identified April 17, 2026More sedimentary →

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Physical properties

Hardness: 7 on Mohs scale; Color: Brownish-tan with a pinkish band; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed by the precipitation of silica in sedimentary environments, often replacing calcium carbonate in limestone or through the accumulation of siliceous organic remains (like diatoms or radiolarians). Formation can range from the Precambrian to Cenozoic eras.

Uses & applications

Historically used for making stone tools (arrowheads, knives) due to its sharp edges when fractured. Modern uses include road surfacing, jewelry (when colorful), and fire-starting tools (flint and steel).

Geological facts

Chert is so durable that it often survives much longer than the host rocks it formed in, which is why it is frequently found as pebbles in stream beds. The pink banding in this specimen is likely due to trace impurities of iron oxide (hematite).

Field identification & locations

Identify in the field by its hardness (will scratch glass), waxy feel, and smooth, shell-like (conchoidal) fracture patterns. It is common worldwide in limestone-heavy regions.