sedimentary

Chert (Nodule)

Microcrystalline Quartz (SiO2)

Hardness: 6.5-7 on Mohs scale; Color: Tan, brown, or gray; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness: 6
Color: Tan, brown, or gray
Luster: Dull to waxy

Identified May 6, 2026More sedimentary →

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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Tan, brown, or gray; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic remains or chemical precipitation within sedimentary host rocks like limestone. Often found in Phanerozoic age strata.

Uses & applications

Used historically for stone tools due to its sharp edges; modern uses include road surfacing, construction aggregates, and occasionally as a semi-precious gemstone when colorful.

Geological facts

Chert was one of the most vital resources for prehistoric humans for making arrowheads and scrapers. The concentric banding visible in this specimen is typical of silica replacement patterns.

Field identification & locations

Identify in the field by its hardness (it will scratch glass) and its shell-like conchoidal fracture. Common in gravel pits and limestone outcrops. Collectors look for unique banding or internal patterns.