Rock Identifier
Chert / Chalcedony Nodules (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert / Chalcedony Nodules

Silicon Dioxide (SiO2)

Hardness: 6.5-7 (Mohs scale); Color: Tan, beige, brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Conchoidal fracture; Specific gravity: 2.6-2.65.

Hardness
6
Color
Tan, beige, brown
Luster
Waxy to dull
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Tan, beige, brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Conchoidal fracture; Specific gravity: 2.6-2.65.

Formation & geological history

Formed by the precipitation of silica from groundwater or within sedimentary rock layers like limestone or chalk. Often accumulates in nodules during the diagenesis of oceanic sediments.

Uses & applications

Historically used for stone tools and arrowheads; currently used in jewelry (as agate or jasper variants), as landscape stone, or as a source for high-purity silica.

Geological facts

Chert was one of the first materials used by early humans to create sharp tools due to its conchoidal fracture pattern. It is highly resistant to chemical weathering.

Field identification & locations

Identify by its extreme hardness (will scratch glass), waxy feel, and smooth, curved (conchoidal) breakage. Commonly found in riverbeds or eroding out of limestone cliffs.