Rock Identifier
Mixed collection of polished pebbles, including probable fossiliferous limestone (Unidentified sedimentary rocks; the gray pebble with circular fossils may be bioclastic limestone) — sedimentary
sedimentary

Mixed collection of polished pebbles, including probable fossiliferous limestone

Unidentified sedimentary rocks; the gray pebble with circular fossils may be bioclastic limestone

AI-generated identification · may be incorrect

Rounded, polished specimens show mottled brown, gray, cream, and black patterns, with apparent fossil fragments in some. Exact hardness, mineral composition, and crystal structure cannot be determined from the image; limestone is typically calcite-rich, Mohs 3, with a nonmetallic luster.

Identified More sedimentary →
Explore Mixed collection of polished pebbles, including probable fossiliferous limestone in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Rounded, polished specimens show mottled brown, gray, cream, and black patterns, with apparent fossil fragments in some. Exact hardness, mineral composition, and crystal structure cannot be determined from the image; limestone is typically calcite-rich, Mohs 3, with a nonmetallic luster.

Formation & geological history

The pebbles likely formed as sedimentary rocks from deposited mineral grains and/or shell material, then were rounded by water and polished. Their geological ages and original environments cannot be established from appearance alone.

Uses & applications

Suitable for collecting, display, or decorative crafts; limestone may also be used in cement and aggregate.

Geological facts

The circular markings on the lower gray stone may be fossil cross-sections, but visual confirmation would require closer examination.

Field identification & locations

Look for fossil patterns, grain texture, and acid reaction (calcite-rich limestone may fizz with dilute acid). Similar pebbles occur in riverbeds, beaches, and sedimentary-rock regions worldwide.