Rock Identifier
Fossiliferous limestone (Bioclastic calcarenite/calcirudite, primarily calcite (CaCO₃)) — sedimentary
sedimentary

Fossiliferous limestone

Bioclastic calcarenite/calcirudite, primarily calcite (CaCO₃)

AI-generated identification · may be incorrect

Cream to tan, granular matrix with abundant shell or coral fragments; dull to slightly sugary luster, generally massive, Mohs hardness 3, and specific gravity about 2.6–2.8. Calcite-rich areas effervesce strongly with dilute hydrochloric acid.

Identified More sedimentary
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Physical properties

Cream to tan, granular matrix with abundant shell or coral fragments; dull to slightly sugary luster, generally massive, Mohs hardness 3, and specific gravity about 2.6–2.8. Calcite-rich areas effervesce strongly with dilute hydrochloric acid.

Formation & geological history

Forms when marine shells, skeletal debris, or reef material accumulate, become compacted, and cemented on a shallow seafloor; age cannot be determined from the image and may range from Paleozoic to Cenozoic. Later uplift exposes the rock at the surface.

Uses & applications

Used as crushed aggregate, cement and lime feedstock, building stone, decorative stone, and educational or fossil-collecting specimens; porous pieces may be polished or cut.

Geological facts

The visible elongated white structures are likely fragmented shells or colonial coral rather than crystals. Fossil-rich limestone records ancient marine environments and can preserve ecological information.

Field identification & locations

Common in former shallow-marine basins worldwide, including Florida, the Caribbean, the Mediterranean, and many other carbonate provinces. Confirm by acid testing and examining fragments for shell growth lines or coral structure; avoid acid if preservation is important.