
sedimentary
Fossiliferous limestone pebble
Bioclastic limestone, primarily calcite (CaCO₃)
AI-generated identification · may be incorrectTan, fine-grained matrix with visible shell or fossil fragments; typically dull to slightly earthy luster, Mohs hardness 3, and poor crystalline visibility. Calcite-rich limestone fizzes readily with dilute hydrochloric acid or strong vinegar, though weathering may reduce the reaction.
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Physical properties
Tan, fine-grained matrix with visible shell or fossil fragments; typically dull to slightly earthy luster, Mohs hardness 3, and poor crystalline visibility. Calcite-rich limestone fizzes readily with dilute hydrochloric acid or strong vinegar, though weathering may reduce the reaction.
Formation & geological history
Formed from accumulated and cemented marine skeletal debris, likely deposited in a shallow tropical sea during the Paleozoic–Cenozoic (exact age requires fossil identification). Later erosion rounded it into a pebble.
Uses & applications
Used as aggregate, cement and lime feedstock, building stone, and ornamental material; this small specimen has mainly educational or collecting value.
Geological facts
The pale inclusions may be shell fragments, but a clear identification requires magnification and possibly thin-section study. Fossiliferous limestone can preserve brachiopods, bivalves, crinoids, or other marine organisms.
Field identification & locations
Common in sedimentary terrains, river gravels, beaches, and limestone quarries worldwide. Look for bedding, fossil outlines, earthy texture, and acid effervescence; avoid confusing it with fossil-bearing concrete.
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