sedimentary

Chert (Nodular Chert)

Microcrystalline or cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

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

Hardness: 7 on Mohs scale
Color: Reddish-brown, tan, or gray
Luster: Dull to waxy

Identified April 13, 2026More sedimentary →

Explore Chert (Nodular Chert) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

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

Formation & geological history

Formed through the chemical precipitation of silica-rich fluids or by the replacement of calcium carbonate in limestone by silica. Common in marine deposits ranging from Precambrian to Cenozoic ages.

Uses & applications

Historically used for stone tools (arrowheads). Modernly used in road construction, as an abrasive, and sometimes in landscaping or basic lapidary work.

Geological facts

Chert is so hard it can create sparks when struck against steel. It is one of the most durable rocks on Earth and survives intense weathering, which is why it's often found as river pebbles.

Field identification & locations

Identify in the field by its extreme hardness (will scratch glass and steel), smooth conchoidal (shell-like) fracture edges, and waxy texture. Frequently found in limestone outcrops or as river bed-load.