Rock Identifier
Small clear-to-milky quartz fragment (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Small clear-to-milky quartz fragment

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

Translucent, colorless to milky, with a vitreous luster; hardness 7 Mohs, trigonal crystal system, and no true cleavage. The small, blocky shape and reflections make exact identification uncertain from the photo.

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Physical properties

Translucent, colorless to milky, with a vitreous luster; hardness 7 Mohs, trigonal crystal system, and no true cleavage. The small, blocky shape and reflections make exact identification uncertain from the photo.

Formation & geological history

Quartz forms in igneous and metamorphic rocks and in hydrothermal veins, crystallizing from silica-rich melts or fluids over geologic time.

Uses & applications

Quartz is used in glass, electronics, abrasives, and jewelry; this tiny fragment has mainly modest collecting or craft value.

Geological facts

Quartz is one of Earth’s most abundant minerals and commonly occurs in many rock types.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch glass, and conchoidal fracture; common worldwide in veins, granites, and pegmatites.