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

Weathered quartz-rich metamorphic rock, likely quartzite

Quartzite; predominantly quartz (SiO₂), possibly with feldspar, mica, and iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 7 Mohs; pale gray, white, and rusty brown, with a granular sugary texture and dull to glassy luster. Quartzite lacks prominent cleavage and commonly breaks irregularly; the image is insufficient for definitive identification.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs; pale gray, white, and rusty brown, with a granular sugary texture and dull to glassy luster. Quartzite lacks prominent cleavage and commonly breaks irregularly; the image is insufficient for definitive identification.

Formation & geological history

Forms when quartz-rich sandstone is recrystallized under heat and pressure during regional metamorphism, commonly in Precambrian to younger mountain belts. Surface iron oxidation produces the brown staining and weathered rind.

Uses & applications

Used as crushed aggregate, road stone, building stone, landscaping rock, and occasionally countertops or decorative slabs. Ordinary weathered pieces have little commercial value.

Geological facts

Quartzite is generally harder and more resistant to weathering than its sandstone precursor. A useful test is that a steel nail usually will not scratch fresh quartzite, whereas quartz-rich sandstone may crumble or scratch more readily.

Field identification & locations

Common in metamorphic terrains, river gravels, glacial deposits, and mountain foothills worldwide. Look for fused quartz grains and a lack of obvious sand-grain boundaries; acid reaction should be absent unless carbonate minerals are present.