Rock Identifier
Fossiliferous limestone with shell fragments (Bioclastic calcarenite; predominantly calcite (CaCO₃), with fossil mollusk material) — sedimentary
sedimentary

Fossiliferous limestone with shell fragments

Bioclastic calcarenite; predominantly calcite (CaCO₃), with fossil mollusk material

AI-generated identification · may be incorrect

Typically Mohs hardness 3, white to cream or gray, dull to sugary/vitreous on fresh shell surfaces, and nonfoliated. Calcite commonly fizzes strongly with dilute hydrochloric acid; visible curved shell layers and porous cement are diagnostic.

Identified More sedimentary
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Physical properties

Typically Mohs hardness 3, white to cream or gray, dull to sugary/vitreous on fresh shell surfaces, and nonfoliated. Calcite commonly fizzes strongly with dilute hydrochloric acid; visible curved shell layers and porous cement are diagnostic.

Formation & geological history

Formed when marine shells and carbonate skeletal debris accumulated, were compacted, and cemented on a shallow seafloor. The exact age cannot be determined from the photograph; such limestones range from Paleozoic to Quaternary.

Uses & applications

Used as building stone, aggregate, cement and lime feedstock; attractive fossil-bearing pieces are collected or displayed rather than used as gemstones.

Geological facts

The specimen appears dominated by recrystallized or broken shell fragments in a carbonate matrix, possibly including bivalve or gastropod material. Acid testing on an inconspicuous area helps distinguish it from silicate rock.

Field identification & locations

Common in marine sedimentary basins worldwide, including Florida, the Bahamas, Mediterranean regions, and many coastal platforms. Look for fossils, powdery carbonate surfaces, low density, and vigorous acid effervescence.