sedimentary

Chert (Common Opal variant)

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5–7 on Mohs scale; Color: Creamy yellowish-beige with white streaks; Luster: Waxy to sub-vitreous; Crystal Structure: Amorphous/Microcrystalline (Cryptocrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.1–2.2.

Hardness: 6
Color: Creamy yellowish-beige with white streaks
Luster: Waxy to sub-vitreous

Identified April 17, 2026More sedimentary →

Explore Chert (Common Opal variant) 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 through the precipitation of silica-rich fluids in sedimentary environments. Often results from the accumulation of siliceous organisms or the replacement of other minerals. This specimen appears to be a weathered fragment likely from a secondary deposit.

Uses & applications

While low-grade specimens like this are mostly for personal collections, higher quality chert and common opal are used for lapidary work (cabs), tumbling, and historically for making stone tools (arrowheads).

Geological facts

Chert is one of the most durable sedimentary rocks. In its waxy, opaque form, it is closely related to flint and jasper. Unlike precious opal, common opal like this does not show a 'play of color' due to the random arrangement of silica spheres.

Field identification & locations

Identify in the field by its waxy texture, conchoidal (shell-like) fracture edges, and the fact that it can scratch glass. This specific color is common in arid environments where silica precipitates in soil or volcanic ash layers.