
metamorphic
Likely quartzite
Quartzite, composed predominantly of quartz (SiO₂)
AI-generated identification · may be incorrectThe rough, tan-gray specimen has pale streaks and a dull to slightly glassy surface. Quartz has Mohs hardness 7 and trigonal crystal structure; grain size and cleavage are not clear in this image.
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Physical properties
The rough, tan-gray specimen has pale streaks and a dull to slightly glassy surface. Quartz has Mohs hardness 7 and trigonal crystal structure; grain size and cleavage are not clear in this image.
Formation & geological history
Quartzite forms when quartz-rich sandstone is recrystallized by heat and pressure during metamorphism. Its age and precise formation setting cannot be determined from the photograph.
Uses & applications
Used as crushed stone, building and decorative stone, and sometimes as a lapidary material.
Geological facts
Quartzite is typically much harder and more resistant to weathering than its sandstone precursor.
Field identification & locations
A likely quartzite; confirm by testing whether it scratches glass and whether grains remain fused rather than crumbling. Quartzite occurs in metamorphic belts worldwide; the specimen’s location is unknown.
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