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.

Identified More mineral
Explore Rounded white pebble, likely quartz or feldspar in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

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.