Rock Identifier
Weathered quartz-rich metamorphic rock, likely quartzite (Quartzite; predominantly microcrystalline quartz (SiO₂), possibly with feldspar, mica, and iron-oxide staining) — metamorphic
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 incorrect

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.

Identified More metamorphic
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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.