Rock Identifier
White quartz pebble (probable) (Quartz, silicon dioxide (SiO₂)) — mineral
mineral

White quartz pebble (probable)

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Small rounded, opaque-to-translucent white pebble with a dull to weakly vitreous luster; likely hardness Mohs 7, no cleavage, conchoidal fracture, and specific gravity about 2.65. The smooth shape indicates water or abrasion wear, though the image cannot confirm composition.

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Physical properties

Small rounded, opaque-to-translucent white pebble with a dull to weakly vitreous luster; likely hardness Mohs 7, no cleavage, conchoidal fracture, and specific gravity about 2.65. The smooth shape indicates water or abrasion wear, though the image cannot confirm composition.

Formation & geological history

Likely derived from quartz-rich igneous or metamorphic rock and rounded by stream, beach, or sediment transport. Quartz commonly formed in veins, granitic rocks, and metamorphic environments over diverse geological ages.

Uses & applications

Common quartz pebbles are used decoratively, in landscaping, aggregate, and occasionally crafts; this small specimen has negligible commercial or jewelry value.

Geological facts

White coloration usually results from microscopic fluid inclusions, fractures, or fine grain boundaries rather than a different quartz species. Similar-looking white pebbles can also be calcite, marble, porcelain, or coated material.

Field identification & locations

Test cautiously: quartz scratches ordinary glass and is not scratched by a steel knife; calcite does not scratch glass and fizzes in dilute acid. Common worldwide, especially in river gravels, beaches, and quartz-vein areas.