
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 incorrectWhite 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.
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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.
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