
metamorphic
Iron-stained quartz-rich rock, possibly quartzite
Quartz-rich rock dominated by silicon dioxide (SiO₂), with red iron-oxide staining; exact rock type is uncertain from the image
AI-generated identification · may be incorrectOpaque, rough, white to salmon-red, with a dull to slightly vitreous luster and no obvious cleavage. Quartz has Mohs hardness 7 and hexagonal crystal structure; the specimen’s grain size and specific gravity cannot be determined from the photo.
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Physical properties
Opaque, rough, white to salmon-red, with a dull to slightly vitreous luster and no obvious cleavage. Quartz has Mohs hardness 7 and hexagonal crystal structure; the specimen’s grain size and specific gravity cannot be determined from the photo.
Formation & geological history
Likely formed from quartz-rich material and colored by iron oxides; if quartzite, it formed through metamorphism of sandstone. Its geological age and precise formation environment cannot be established visually.
Uses & applications
Quartzite is used as aggregate, construction stone, and sometimes decorative stone; this rough fragment has little apparent jewelry value.
Geological facts
Red and orange tones commonly result from hematite or other iron-oxide coatings or inclusions.
Field identification & locations
Look for abundant hard quartz grains and test whether it scratches glass; quartzite typically resists scratching and does not fizz in dilute acid. Similar material occurs widely in regions with quartz-rich sandstone or metamorphic rocks.
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