
metamorphic
Reddish-purple river pebble, likely quartzite
Quartzite, composed mainly of quartz (SiO₂); exact identification is uncertain from the image alone.
AI-generated identification · may be incorrectFine-grained, opaque, muted reddish-purple with a smooth, rounded surface; quartzite typically has Mohs hardness 7, a nonmetallic luster, and no cleavage. The pictured stone’s grain and texture are not clear enough to confirm its mineral makeup.
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Physical properties
Fine-grained, opaque, muted reddish-purple with a smooth, rounded surface; quartzite typically has Mohs hardness 7, a nonmetallic luster, and no cleavage. The pictured stone’s grain and texture are not clear enough to confirm its mineral makeup.
Formation & geological history
Quartzite forms when quartz-rich sandstone is recrystallized by heat and pressure during metamorphism. Such pebbles are often rounded through transport in rivers or coastal settings; its geological age cannot be determined from appearance.
Uses & applications
Commonly used as decorative landscaping stone, aggregate, and occasionally as a lapidary material when attractive or unusually colored.
Geological facts
Iron-bearing minerals can lend quartzite red or purple hues. A useful check is whether it scratches glass and resists scratching by a steel knife, though these tests are not definitive.
Field identification & locations
Look for a hard, dense pebble with interlocking quartz grains and no obvious layering; quartzite occurs worldwide and commonly accumulates in river gravel. The image does not show enough detail to distinguish it confidently from other fine-grained rocks.
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