sedimentary

Banded Chert (Jasper)

Silicon Dioxide (SiO2)

Hardness: 6.5–7 (Mohs scale); Color: Gray, brown, black, and tan horizontal banding; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.6–2.7

Hardness: 6
Color: Gray, brown, black, and tan horizontal banding
Luster: Waxy to vitreous

Identified April 20, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation from sea water. The banding occurs due to rhythmic changes in sediment supply or oxygen levels during deposition millions of years ago, often in deep-sea environments.

Uses & applications

Used historically for stone tools (flintknapping) due to its sharp conchoidal edges. Today, primarily used as lapidary material for polishing, cabochons, and decorative stones in aquariums or landscaping.

Geological facts

Banded chert is often associated with the oldest fossils on Earth. Banded Iron Formations (BIFs) are a specific type of banded chert that contain high levels of hematite or magnetite, recording the rise of oxygen in Earth's atmosphere billions of years ago.

Field identification & locations

Identify in the field by its smooth, glass-like texture and its inability to be scratched by a steel knife. It often feels 'slicker' than surrounding sandstone or limestone. Look for distinctive parallel layers and shell-like (conchoidal) fractures where the rock has chipped.