
metamorphic
Likely weathered quartz-rich rock (possibly quartzite or milky quartz pebble)
Quartzite; predominantly quartz (SiO₂), but exact identification is uncertain from the photograph
AI-generated identification · may be incorrectRounded, light gray-white specimen with a dull to weakly glassy luster and granular texture; likely Mohs hardness ~7, no obvious cleavage, and specific gravity near 2.6. The dark central area may be staining, matrix, or a shadow rather than a distinct mineral.
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Physical properties
Rounded, light gray-white specimen with a dull to weakly glassy luster and granular texture; likely Mohs hardness ~7, no obvious cleavage, and specific gravity near 2.6. The dark central area may be staining, matrix, or a shadow rather than a distinct mineral.
Formation & geological history
If quartzite, it formed when quartz-rich sandstone was recrystallized during metamorphism, commonly in Precambrian to younger mountain belts; if a quartz pebble, it was transported and rounded by erosion. Common in river gravels and weathered outcrops.
Uses & applications
Quartzite is used as aggregate, road stone, building or decorative stone, and occasionally as a lapidary material; ordinary pebbles have little commercial value.
Geological facts
Quartz-rich rocks resist weathering and commonly survive as rounded stream cobbles. A steel knife should not scratch fresh quartz-rich surfaces, though weathered coatings can scratch more easily.
Field identification & locations
Look for interlocking quartz grains, white-gray color, and inability to scratch with a knife; quartzite is generally tougher and more granular than massive quartz. Common in metamorphic terrains and stream deposits.
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