
sedimentary
Fossiliferous Limestone (with Oyster Fossils)
Fossiliferous Calcarenite / Bivalve Mollusk Fossil
AI-generated identification · may be incorrectHardness: 3 (calcite matrix); Color: Gray-buff, tan, and cream; Luster: Dull, earthy; Crystal structure: Amorphous/microcrystalline matrix; Cleavage: None (rhombohedral in calcite crystals within shells)
- Hardness
- 3 (calcite matrix)
- Color
- Gray-buff, tan, and cream
- Luster
- Dull, earthy
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Physical properties
Hardness: 3 (calcite matrix); Color: Gray-buff, tan, and cream; Luster: Dull, earthy; Crystal structure: Amorphous/microcrystalline matrix; Cleavage: None (rhombohedral in calcite crystals within shells)
Formation & geological history
Formed in shallow marine environments where accumulation of calcium carbonate shells occurred. These sediments were buried and lithified via chemical precipitation over millions of years, typically dating from the Cretaceous to Cenozoic eras.
Uses & applications
Used in construction as building stone, in the production of cement, for soil conditioning in agriculture, and as decorative pieces for collectors.
Geological facts
This specimen contains several fossilized oyster shells (Ostreidae). Oysters are known to form dense 'reefs' or beds which, when fossilized, provide excellent records of ancient sea levels and water temperatures.
Field identification & locations
Identify in the field by looking for layered shell fragments and reacting with dilute hydrochloric acid (it will fizz). Commonly found in sedimentary basins and coastal cliffs. Collectors should look for well-preserved hinge segments.
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