Rock Identifier
Rounded white pebble, likely quartz or feldspar (Most consistent with milky quartz (SiO₂), though altered feldspar or calcite is possible from the image) — mineral
mineral

Rounded white pebble, likely quartz or feldspar

Most consistent with milky quartz (SiO₂), though altered feldspar or calcite is possible from the image

AI-generated identification · may be incorrect

White, opaque, smooth and water-rounded, with a dull to faintly vitreous luster; quartz hardness is Mohs 7, feldspar 6–6.5, and calcite 3. It appears massive rather than visibly crystalline and has no obvious cleavage.

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Physical properties

White, opaque, smooth and water-rounded, with a dull to faintly vitreous luster; quartz hardness is Mohs 7, feldspar 6–6.5, and calcite 3. It appears massive rather than visibly crystalline and has no obvious cleavage.

Formation & geological history

Likely a naturally weathered and transported pebble from stream, beach, or gravel; the specimen’s geological age cannot be determined visually. Quartz pebbles commonly derive from erosion of older igneous or metamorphic rocks.

Uses & applications

Small pieces are used as inexpensive curiosities, craft material, or tumbling feed; quartz is also important in glass, electronics, and engineered stone. This individual pebble has minimal commercial value.

Geological facts

The rounded shape indicates abrasion during transport. A quartz identification can be tested with a steel nail or knife (quartz should resist scratching) and by checking for fizz with dilute acid to exclude calcite.

Field identification & locations

Common in river gravels, beaches, and glacial deposits worldwide; likely local material rather than a rare specimen. Confirm with hardness, streak (white), and a loupe examination for cleavage or translucent edges.