fossil

Fossil oyster shell

Fossilized bivalve, likely Ostrea or a related oyster genus; calcite (CaCO₃) shell

AI-generated identification · may be incorrect

Gray-brown, irregularly ribbed and layered surface with dull to slightly pearly luster; calcite hardness ~3, good cleavage, and specific gravity ~2.7. The strongly corrugated, foliated shell texture is characteristic of an oyster rather than crystalline rock.

Identified August 25, 2026More fossil →

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Physical properties

Formation & geological history

A marine bivalve shell was buried in carbonate-rich sediment and mineral-preserved or partially replaced during diagenesis. Exact geological age cannot be determined from the photograph; oyster fossils range from the Jurassic to Recent, commonly in Cretaceous–Cenozoic marine deposits.

Uses & applications

Primarily a collecting, educational, and decorative specimen; fossil shell material is not normally used industrially. Crushed fossil shells may contribute carbonate to local soils or aggregate.

Geological facts

Oysters commonly have one deeply cupped valve and one flatter valve, with growth layers recording environmental changes. Fossil shells may retain original calcite or become heavily recrystallized.

Field identification & locations

Identify it by the irregular oyster-like shape, concentric growth layers, and radiating ribs; dilute vinegar should weakly effervesce on exposed calcite. Common in former shallow-marine limestone, marl, and coastal deposits worldwide.