Rock Identifier
Chert Nodule (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert Nodule

Microcrystalline Quartz (SiO2)

Hardness: 6.5-7 Mohs; Color: Brown and white; Luster: Waxy to dull; Structure: Cryptocrystalline; Fracture: Conchoidal; Specific Gravity: 2.65

Hardness
6
Color
Brown and white
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 Mohs; Color: Brown and white; Luster: Waxy to dull; Structure: Cryptocrystalline; Fracture: Conchoidal; Specific Gravity: 2.65

Formation & geological history

Formed through the replacement of limestone or carbonate sediment by silica-rich fluids. Often occurs as nodules or beds within sedimentary rock layers like limestone or chalk.

Uses & applications

Historically used for stone tools (arrowheads). Today used for landscaping, as a road mineral, or for decorative lapidary work in its more colorful forms (Jasper/Agate).

Geological facts

Chert has been used by humans for millions of years because its conchoidal fracture creates sharp edges perfect for cutting and scraping tools.

Field identification & locations

Identify in the field by its waxy texture, its ability to scratch glass, and the seashell-like curves (conchoidal fracture) when broken. Commonly found in stream beds or eroded limestone outcrops.