
sedimentary
Fossiliferous limestone with shell fragments
Bioclastic calcarenite; predominantly calcite (CaCO₃), with fossil mollusk material
AI-generated identification · may be incorrectTypically 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.
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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.
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