sedimentary

Chert (with Quartz/Chalcedony)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 (Mohs scale); Color: Variegated brown, grey, white, and reddish-orange; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness: 7 (Mohs scale)
Color: Variegated brown, grey, white, and reddish-orange
Luster: Waxy to vitreous

Identified April 13, 2026More sedimentary →

Explore Chert (with Quartz/Chalcedony) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Formed from the accumulation of silica-rich fluids in limestone or through the accumulation of siliceous biological remains (like diatoms or radiolarians). Common in sedimentary basins and often found as nodules or layers.

Uses & applications

Historically used for making stone tools (arrowheads). Modernly used in construction aggregate, as landscaping stone, or as decorative specimens for collectors when polished.

Geological facts

Chert is so hard it can strike sparks against steel. The reddish tints in this specific specimen likely come from iron oxide (hematite) impurities staining the silica.

Field identification & locations

Identify by its waxy appearance and conchoidal (shell-like) fracture patterns when broken. Look for it in limestone or chalk outcrops. Collectors should check for translucency at the edges.