Rock Identifier
Flint / Chert Nodule (Silica (Microcrystalline Quartz), SiO2) — sedimentary
sedimentary

Flint / Chert Nodule

Silica (Microcrystalline Quartz), SiO2

Hardness of 7 on the Mohs scale, typically brown, gray, or black with a waxy to vitreous luster, conchoidal fracture, and no true cleavage.

Identified More sedimentary
Explore Flint / Chert Nodule in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness of 7 on the Mohs scale, typically brown, gray, or black with a waxy to vitreous luster, conchoidal fracture, and no true cleavage.

Formation & geological history

Formed through the replacement of calcium carbonate by silica-rich solutions in marine limestone or chalk environments during the Cretaceous period.

Uses & applications

Historically used for making stone tools, fire-starting strikers, and building materials; today primarily of interest to beachcombers and fossil hunters.

Geological facts

This specimen has been smoothed and shaped by wave action on a beach, giving it a distinctive pebble form while retaining the characteristic knobby or nodular texture of flint.

Field identification & locations

Found worldwide in chalk and limestone deposits, easily identified by its conchoidal fracture, waxy texture, and high hardness which easily scratches glass.