Rock Identifier
Banded Quartz (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Banded Quartz

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, trigonal crystal system, conchoidal fracture, and a specific gravity of 2.65.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, trigonal crystal system, conchoidal fracture, and a specific gravity of 2.65.

Formation & geological history

Formed through the deposition and cementation of quartz-rich sand grains over millions of years, often in ancient beaches or riverbeds.

Uses & applications

Used primarily in lapidary arts, jewelry making, and as a decorative display specimen for mineral collectors.

Geological facts

The distinct bands are caused by mineral impurities such as iron oxides filtering through permeable layers during formation.

Field identification & locations

Identified by its characteristic color banding and resistance to scratching steel; commonly found in sedimentary rock formations worldwide.