Rock Identifier
Rounded river pebble, likely quartz-rich chert or fine-grained sandstone (Indeterminate lithic clast; possible microcrystalline quartz (chert) or quartz-rich sandstone) — sedimentary
sedimentary

Rounded river pebble, likely quartz-rich chert or fine-grained sandstone

Indeterminate lithic clast; possible microcrystalline quartz (chert) or quartz-rich sandstone

AI-generated identification · may be incorrect

Small, naturally water-worn oval with dull earthy gray-brown color, fine texture, and subvitreous to dull luster. Hardness is approximately 6–7 if chert, or 5–6 if sandstone; no obvious cleavage or visible crystals.

Identified More sedimentary
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Physical properties

Small, naturally water-worn oval with dull earthy gray-brown color, fine texture, and subvitreous to dull luster. Hardness is approximately 6–7 if chert, or 5–6 if sandstone; no obvious cleavage or visible crystals.

Formation & geological history

Likely produced by weathering and abrasion in a stream, beach, or glacial deposit; its original sedimentary rock may be millions to hundreds of millions of years old, but age cannot be determined from the photograph.

Uses & applications

Usually a common collecting pebble with negligible commercial value; suitable for crafts, landscaping, or educational reference, but not typically used as an ornamental stone.

Geological facts

The pale speckles and uniform fine grain are compatible with chert, silicified sediment, or weathered quartz-rich sandstone. A scratch test and fresh broken surface would substantially improve identification.

Field identification & locations

Common in stream gravels and beaches worldwide. Chert should scratch glass and resist a steel knife; sandstone is more porous and may shed grains, while dilute acid generally causes no reaction unless carbonate cement is present.