Rock Identifier
Rounded river pebble, likely quartz-rich sandstone or quartzite (Indeterminate; probable quartz (SiO₂) with feldspar, iron-oxide staining, and minor lithic grains) — sedimentary or metamorphic
sedimentary or metamorphic

Rounded river pebble, likely quartz-rich sandstone or quartzite

Indeterminate; probable quartz (SiO₂) with feldspar, iron-oxide staining, and minor lithic grains

AI-generated identification · may be incorrect

Smooth, water-rounded cobble with tan-gray to brown color, earthy-to-dull luster, and fine granular texture; likely Mohs 6–7 if quartz-rich, with no obvious cleavage. Exact identification requires a fresh surface, acid test, and hardness testing.

Identified More sedimentary or metamorphic
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Physical properties

Smooth, water-rounded cobble with tan-gray to brown color, earthy-to-dull luster, and fine granular texture; likely Mohs 6–7 if quartz-rich, with no obvious cleavage. Exact identification requires a fresh surface, acid test, and hardness testing.

Formation & geological history

Formed as a sedimentary sandstone and possibly weakly metamorphosed into quartzite, then rounded by abrasion in a river, beach, or glacial deposit. Its formation age cannot be determined from the photograph.

Uses & applications

Usually a natural specimen, landscaping stone, or craft material; quartzite may be used as aggregate, construction stone, or dimension stone. As shown, it has little jewelry value.

Geological facts

The rounded shape records prolonged transport or wave action, while brown coloration commonly comes from iron oxides. A steel file or knife should not easily scratch a quartz-rich surface.

Field identification & locations

Common worldwide in streambeds and gravel deposits; inspect for visible sand grains, gritty texture, and quartz-rich translucence on a broken edge. A glass-scratching test can support quartz content but is not definitive.