Rock Identifier
Weathered quartz-rich pebble (Likely milky quartz or quartzite (SiO₂), possibly a weathered feldspathic rock) — igneous
igneous

Weathered quartz-rich pebble

Likely milky quartz or quartzite (SiO₂), possibly a weathered feldspathic rock

AI-generated identification · may be incorrect

Off-white, opaque, fine- to medium-grained pebble with dull to weakly vitreous luster and brown surface staining; quartz hardness is about 7 Mohs, with no obvious cleavage. Exact identification is limited by the small, weathered specimen and photograph.

Identified More igneous
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Physical properties

Off-white, opaque, fine- to medium-grained pebble with dull to weakly vitreous luster and brown surface staining; quartz hardness is about 7 Mohs, with no obvious cleavage. Exact identification is limited by the small, weathered specimen and photograph.

Formation & geological history

Likely eroded from quartz vein material, quartzite, or a silica-rich igneous rock and rounded by stream or beach transport; its geological age cannot be determined visually. Iron-oxide staining accounts for the brown patches.

Uses & applications

Common pebbles have little commercial value, though quartzite is used as aggregate, landscaping stone, and construction material; attractive pieces may be collected or tumbled.

Geological facts

Quartz commonly forms durable white pebbles because it resists chemical and physical weathering. A glass-scratch test can help distinguish quartz from softer white minerals, but it may damage the specimen.

Field identification & locations

Look for glassy fracture, lack of cleavage, and inability to scratch it with a steel nail; quartzite may show fused granular texture, while feldspar is softer and often cleaves. Common worldwide in streambeds, beaches, and glacial deposits.