Rock Identifier
Rounded quartz-rich river pebble (Likely quartz arenite or chert-derived sandstone; identification is limited from the photograph) — sedimentary
sedimentary

Rounded quartz-rich river pebble

Likely quartz arenite or chert-derived sandstone; identification is limited from the photograph

AI-generated identification · may be incorrect

Pale tan-gray, fine-grained, dull to weakly silky luster, and smoothly water-worn; likely hardness about 6–7 if quartz-rich, with no visible cleavage. Dense and compact, but grain texture is not resolvable.

Identified More sedimentary
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Physical properties

Pale tan-gray, fine-grained, dull to weakly silky luster, and smoothly water-worn; likely hardness about 6–7 if quartz-rich, with no visible cleavage. Dense and compact, but grain texture is not resolvable.

Formation & geological history

Probably a weathered and stream-rounded sedimentary fragment, formed from cemented sand or silica-rich microcrystalline material; its depositional age cannot be determined visually. Subsequent erosion produced the rounded shape.

Uses & applications

Generally used as a decorative pebble, paperweight, or landscaping stone; it has little jewelry or industrial value unless it proves to be attractive chert, jasper, or another distinctive material.

Geological facts

The specimen may also be a fine-grained quartzite or weathered limestone, since color and texture overlap in a single image. A streak, hardness, acid, and grain test would improve identification.

Field identification & locations

Common in river gravels, beaches, glacial deposits, and weathered sedimentary terrains. Scratch testing with steel or glass, checking for visible grains, and applying dilute hydrochloric acid can distinguish quartz-rich rock from calcite-bearing limestone.