
mineral
Milky quartz pebble
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectWhite 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.
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