Rock Identifier
Banded river pebble, likely weathered sandstone or mudstone (Indeterminate lithic clast; probable quartz-rich sandstone or iron-stained mudstone) — sedimentary
sedimentary

Banded river pebble, likely weathered sandstone or mudstone

Indeterminate lithic clast; probable quartz-rich sandstone or iron-stained mudstone

AI-generated identification · may be incorrect

Gray-brown, rounded and water-worn, with thin darker bands or fractures and a dull to faintly earthy luster. Likely hardness about 4–7 Mohs depending on composition; no visible crystals or strong cleavage.

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Physical properties

Gray-brown, rounded and water-worn, with thin darker bands or fractures and a dull to faintly earthy luster. Likely hardness about 4–7 Mohs depending on composition; no visible crystals or strong cleavage.

Formation & geological history

Formed from compacted sediment and later rounded by stream or beach transport; its precise geological age and source cannot be determined from the photograph. The bands may represent bedding, iron staining, or weathering fractures.

Uses & applications

Primarily a natural curiosity or decorative pebble; not generally valuable for industry, construction, or jewelry unless it proves to be an unusual jasper or other attractive stone.

Geological facts

The smooth shape indicates prolonged abrasion during transport. A close inspection of the bands and a fresh surface would help distinguish sedimentary bedding from cracks or mineral veins.

Field identification & locations

Common in riverbeds, beaches, and gravel deposits worldwide. Test for grain texture, streak, acid reaction, and hardness; a hand lens and fresh break are more diagnostic than surface color.