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

Quartz (Tumbled)

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white or translucent, vitreous to greasy luster, hexagonal crystal system (though not visible in this tumbled form), conchoidal fracture, specific gravity of 2.65.

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Physical properties

Hardness of 7 on the Mohs scale, typically white or translucent, vitreous to greasy luster, hexagonal crystal system (though not visible in this tumbled form), conchoidal fracture, specific gravity of 2.65.

Formation & geological history

Formed in various geological environments including igneous, metamorphic, and sedimentary rocks, often crystallized from silica-rich hydrothermal veins over millions of years.

Uses & applications

Commonly used in jewelry, lapidary arts, decorative items, and metaphysical practices. Industrial uses include electronics, glassmaking, and precision instruments.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust and is well known for its piezoelectric properties.

Field identification & locations

Easily identified by its high hardness (scratches glass) and conchoidal fracture. Found worldwide in nearly every geological setting.