Rock Identifier
Weathered quartz-rich pebble (probable quartzite or quartz vein fragment) (Quartzite, predominantly silicon dioxide (SiO₂); exact identification is uncertain from the photograph) — metamorphic
metamorphic

Weathered quartz-rich pebble (probable quartzite or quartz vein fragment)

Quartzite, predominantly silicon dioxide (SiO₂); exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

White to pale gray, dull-to-waxy luster, fine granular texture, and rounded weathered form; quartz hardness is about Mohs 7, with no obvious cleavage and conchoidal-to-uneven fracture.

Identified More metamorphic
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Physical properties

White to pale gray, dull-to-waxy luster, fine granular texture, and rounded weathered form; quartz hardness is about Mohs 7, with no obvious cleavage and conchoidal-to-uneven fracture.

Formation & geological history

Likely derived from erosion of quartzite or a quartz vein, then naturally rounded by stream or shoreline transport; its original formation may date from Precambrian to younger regional bedrock, depending on locality.

Uses & applications

Common specimens have little commercial value; quartzite is used as crushed aggregate, road stone, building stone, and occasionally as a decorative material.

Geological facts

The tan or brown markings may be iron-oxide staining or attached weathering residue. A steel knife should not scratch it, while quartz or glass can scratch it.

Field identification & locations

Look for uniformly hard, quartz-granular texture and resistance to scratching; vinegar will not visibly react. Common worldwide in gravel beds, stream channels, beaches, and quartz-bearing terrains.