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

Tumbled Quartz

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and trigonal crystal system. Color ranges from milky white to translucent with brownish dendritic inclusions.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and trigonal crystal system. Color ranges from milky white to translucent with brownish dendritic inclusions.

Formation & geological history

Formed via hydrothermal processes where silica-rich fluids precipitate in fractures within Earth's crust. Geological age varies widely depending on the specific deposit.

Uses & applications

Used widely in lapidary arts, jewelry, decorative tumbled stones, and electronic oscillator components.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust and exhibits piezoelectric properties. Dendritic patterns are typically manganese or iron oxides.

Field identification & locations

Identified by its high hardness (scratches glass), lack of cleavage, and waxy-to-vitreous luster on tumbled surfaces. Common worldwide in riverbeds and pegmatites.