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

White to gray, granular and strongly weathered, with dull to weakly glassy luster; quartz hardness is about Mohs 7, no obvious cleavage, and quartzite has an interlocking crystalline texture. The rounded shape and surface discoloration indicate abrasion and weathering.

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Physical properties

White to gray, granular and strongly weathered, with dull to weakly glassy luster; quartz hardness is about Mohs 7, no obvious cleavage, and quartzite has an interlocking crystalline texture. The rounded shape and surface discoloration indicate abrasion and weathering.

Formation & geological history

Forms when quartz-rich sandstone is recrystallized under heat and pressure, commonly during mountain-building; its exact geological age cannot be determined from the photograph. It may have later been transported as a river or glacial cobble.

Uses & applications

Used as crushed stone, aggregate, road material, riprap, and building or decorative stone; attractive dense pieces may be polished, though this specimen appears ordinary and heavily weathered.

Geological facts

Quartzite commonly resists scratching by a steel knife and typically breaks across quartz grains rather than around them. A vinegar test is generally negative, helping distinguish it from limestone or marble.

Field identification & locations

Common in metamorphic mountain belts and stream gravels worldwide. Confirm by checking that grains are fused, the rock does not fizz with dilute acid, and a steel tool fails to scratch it; the image alone cannot exclude hard sandstone or light-colored granite.