Rock Identifier
Milky quartz pebble (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Milky quartz pebble

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

White to translucent, with a vitreous-to-waxy luster and irregular fracture; hardness 7 Mohs, trigonal crystal structure, no cleavage. The specimen appears small and rounded, likely naturally worn or tumbled.

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Physical properties

White to translucent, with a vitreous-to-waxy luster and irregular fracture; hardness 7 Mohs, trigonal crystal structure, no cleavage. The specimen appears small and rounded, likely naturally worn or tumbled.

Formation & geological history

Quartz forms when silica-rich fluids crystallize in veins and cavities, or during igneous and metamorphic processes. Its age cannot be determined from the image; quartz is common in rocks of many geological ages.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and decorative objects; attractive pieces may be used in jewelry or collections.

Geological facts

Milky appearance results from tiny fluid or gas inclusions that scatter light.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch ordinary glass, and lack of cleavage; common worldwide in veins, pegmatites, and river gravels. The image alone cannot confirm quartz, though its appearance is consistent with it.