Rock Identifier
Polished gray stone, likely quartzite or river-worn granite (Tentatively quartzite (mostly microcrystalline SiO₂); exact identification is uncertain from the photograph) — metamorphic
metamorphic

Polished gray stone, likely quartzite or river-worn granite

Tentatively quartzite (mostly microcrystalline SiO₂); exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Smooth, rounded, and weakly lustrous with gray, tan, and brown mottling. Likely hardness about 6.5–7 Mohs, with no obvious cleavage; quartzite has a granular interlocking crystal texture, while granite would show visible quartz and feldspar grains.

Identified More metamorphic
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Physical properties

Smooth, rounded, and weakly lustrous with gray, tan, and brown mottling. Likely hardness about 6.5–7 Mohs, with no obvious cleavage; quartzite has a granular interlocking crystal texture, while granite would show visible quartz and feldspar grains.

Formation & geological history

Probably naturally water-worn and possibly polished; quartzite forms when sandstone is metamorphosed under heat and pressure, commonly during Precambrian to younger mountain-building events. A river pebble could also be weathered granite or another silicate rock.

Uses & applications

Suitable as a decorative pebble, paperweight, or craft/tumbling material; not gem-quality based on the visible appearance. Common specimens are generally inexpensive.

Geological facts

The image does not show diagnostic crystal faces or grain detail, so mineral identification is provisional. A glass-scratch test and close inspection with magnification would distinguish quartzite from softer rocks.

Field identification & locations

Common in river gravels and glacial deposits worldwide. If it scratches ordinary glass and shows fused-looking grains, quartzite is likely; visible pink/white feldspar and translucent quartz suggest granite. Avoid destructive testing if it is a valued specimen.