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

Quartz Nodule

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Mohs hardness of 7, vitreous luster, conchoidal fracture, and lack of cleavage. Color ranges from clear to milky white, gray, or brownish hues.

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Physical properties

Mohs hardness of 7, vitreous luster, conchoidal fracture, and lack of cleavage. Color ranges from clear to milky white, gray, or brownish hues.

Formation & geological history

Formed via hydrothermal precipitation or low-temperature groundwater deposition in cavities, often within sedimentary or igneous host rocks.

Uses & applications

Used in electronics, glassware, ornamental displays, and as a tumbling rough for lapidary work.

Geological facts

Quartz is one of the most abundant minerals in Earth's continental crust and exhibits strong piezoelectric properties.

Field identification & locations

Identify by its hardness (scratches glass), lack of cleavage, and conchoidal fracture. Commonly found globally in pegmatites, veins, and river gravels.