sedimentary

Chert (Nodule)

Chert (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5-7 (Mohs scale); Color: Typically gray, brown, or white; Luster: Waxy to dull; Structure: Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness: 6
Color: Typically gray, brown, or white
Luster: Waxy to dull

Identified April 25, 2026More sedimentary →

Explore Chert (Nodule) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Typically gray, brown, or white; Luster: Waxy to dull; Structure: Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or by chemical precipitation from groundwater within limestone or chalk beds. Most common in ancient oceanic sedimentary environments.

Uses & applications

Historically used for stone tools (arrowheads, scrapers) due to its sharp edges; modernly used in road construction, as jewelry (if colorful), and as fire-starting flints.

Geological facts

Chert is so hard it can scratch glass and sparks when struck against steel. Ancient civilizations preferred it for 'knapping' tools because it breaks in predictable, sharp patterns.

Field identification & locations

Identify in the field by its smooth, waxy feel and distinct conchoidal (shell-like) fracture edges. Commonly found in limestone outcrops or as river-worn pebbles. For collectors, look for translucency or banding.