Rock Identifier
Fossilized Shell in Limestone (Bivalve fossil (CaCO3) in Carbonate Sedimentary Rock) — sedimentary
sedimentary

Fossilized Shell in Limestone

Bivalve fossil (CaCO3) in Carbonate Sedimentary Rock

Hardness: 3-4 (Mohs), Color: Light gray to tan with darker carbonaceous streaks, Luster: Dull/Earthy, Crystal Structure: Microcrystalline calcite with organic preservation, Cleavage: None/Irregular

Identified More sedimentary

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Physical properties

Hardness: 3-4 (Mohs), Color: Light gray to tan with darker carbonaceous streaks, Luster: Dull/Earthy, Crystal Structure: Microcrystalline calcite with organic preservation, Cleavage: None/Irregular

Formation & geological history

Formed by the accumulation of organic debris and calcium carbonate shells in a shallow marine environment over millions of years, typically during the Paleozoic or Mesozoic eras.

Uses & applications

Primarily used in construction (countertops, tiling), as a source of lime, and for paleontological study or decorative fossil collecting.

Geological facts

The shell visible is a bivalve, a member of the class of mollusks that includes clams and oysters. Fossils provide a snapshot of prehistoric marine ecosystems.

Field identification & locations

Identify in the field by looking for concentric growth rings on embedded shapes and the presence of calcite veining or reaction to dilute hydrochloric acid. Common in ancient seabed outcrops.