Rock Identifier
Quartz cluster (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Quartz cluster

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

The specimen appears to be a milky-to-clear quartz cluster with translucent, glassy surfaces and irregular crystal growth. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and a specific gravity of about 2.65.

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Physical properties

The specimen appears to be a milky-to-clear quartz cluster with translucent, glassy surfaces and irregular crystal growth. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and a specific gravity of about 2.65.

Formation & geological history

Quartz forms when silica-rich fluids crystallize in fractures, cavities, or veins; it occurs in rocks of many ages and geological settings. The photo does not reveal its precise geological age or locality.

Uses & applications

Quartz is used in glass and electronics, while attractive clusters are collected or displayed as decorative specimens.

Geological facts

Quartz is one of Earth’s most abundant minerals and can occur in many colors depending on impurities and inclusions.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch ordinary glass, and lack of cleavage; the image alone cannot confirm the identification. Similar pale minerals, especially calcite, can be distinguished by calcite’s lower hardness and acid reaction.