Rock Identifier
Quartz Nodule (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz Nodule

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, grayish-white color, vitreous to waxy luster, and conchoidal fracture.

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Physical properties

Hardness of 7 on the Mohs scale, grayish-white color, vitreous to waxy luster, and conchoidal fracture.

Formation & geological history

Formed through the precipitation of silica from groundwater within cavity linings or sedimentary host rocks over millions of years.

Uses & applications

Used in lapidary arts, decorative items, mineral collections, and as a raw material for industrial silica.

Geological facts

Nodules often form in limestone or chalk beds, protecting the inner quartz or chalcedony from weathering.

Field identification & locations

Identify by its high hardness, inability to be scratched by steel, and waxy or glassy texture on broken surfaces. Commonly found in creek beds and sedimentary formations.