
metamorphic
Weathered quartz-rich metamorphic rock, likely quartzite
Quartzite; predominantly microcrystalline quartz (SiO₂), possibly with feldspar, mica, and iron-oxide staining
AI-generated identification · may be incorrectHardness about 7 Mohs; pale gray to cream with rusty red-brown patches, dull to weakly vitreous luster, massive granular texture, and no obvious cleavage. The irregular rounded shape and weathered surface suggest natural abrasion and oxidation.
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Physical properties
Hardness about 7 Mohs; pale gray to cream with rusty red-brown patches, dull to weakly vitreous luster, massive granular texture, and no obvious cleavage. The irregular rounded shape and weathered surface suggest natural abrasion and oxidation.
Formation & geological history
Formed when quartz-rich sandstone was recrystallized under heat and pressure, commonly during regional mountain-building; its exact geological age cannot be determined from the photograph. It may represent a resistant glacial or stream-transported cobble.
Uses & applications
Used as crushed aggregate, road stone, building stone, and decorative facing; attractive pieces may be polished, though this specimen appears ordinary and unworked.
Geological facts
Quartzite commonly breaks across quartz grains rather than around them, making it tougher than sandstone. Iron oxides produce the reddish staining visible here.
Field identification & locations
Common in metamorphic terrains and glacial deposits. Test with a steel nail or glass: genuine quartzite resists scratching and can scratch glass; acid produces no reaction unless carbonate contamination is present.
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