sedimentary

Chert (Red/Brown Variety)

Microcrystalline quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5-7 (Mohs scale). Color: Brownish-red to tan. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific gravity: 2.6-2.7.

Hardness: 6
Color: Brownish-red to tan
Luster: Waxy to dull

Identified April 13, 2026More sedimentary →

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Physical properties

Hardness: 6.5-7 (Mohs scale). Color: Brownish-red to tan. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific gravity: 2.6-2.7.

Formation & geological history

Formed through the accumulation of silica-rich microfossils (like radiolarians or diatoms) or by the precipitation of silica from groundwater within sedimentary layers like limestone or chalk. It can date from the Precambrian to recent eras.

Uses & applications

Historically used for stone tools (knapping) due to its sharp edges. Today used as decorative gravel, in road construction, and occasionally for lapidary work if highly colored.

Geological facts

Red chert is often colored by iron oxide (hematite). Because of its hardness and chemical stability, it is incredibly resistant to weathering and often found as rounded river pebbles long after the surrounding rock has eroded.

Field identification & locations

Identify by its waxy texture and conchoidal (shell-like) fracture pattern. It will easily scratch glass. Commonly found in riverbeds, beaches, and sedimentary outcrops globally.