Rock Identifier
Chert Nodule (Microcrystalline Quartz) — sedimentary
sedimentary

Chert Nodule

Microcrystalline Quartz

AI-generated identification · may be incorrect

Hardness: 6.5-7 (Mohs), Color: Cream, tan, gray, brown, Luster: Waxy to dull, Fracture: Conchoidal

Hardness
6
Luster
Waxy to dull, Fracture: Conchoidal
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 (Mohs), Color: Cream, tan, gray, brown, Luster: Waxy to dull, Fracture: Conchoidal

Formation & geological history

Formed by the chemical precipitation of silica in sedimentary environments, often within limestone or chalk deposits. Commonly found as nodules or concretions.

Uses & applications

Historically used for making stone tools (flintknapping) due to its conchoidal fracture. Sometimes used as a low-grade aggregate or in landscaping.

Geological facts

Chert and flint are closely related, with flint specifically referring to dark chert found in chalk. The sharp edges created when broken made it a crucial material for early human tools and weapons.

Field identification & locations

Identify by its hardness (scratches glass), waxy luster, and conchoidal fracture. Often found as rounded or irregular nodules eroding out of limestone.