Rock Identifier
Fossiliferous Limestone (Coquina / Shell Conglomerate) (Bioclastic Limestone (composed primarily of CaCO3)) — sedimentary
sedimentary

Fossiliferous Limestone (Coquina / Shell Conglomerate)

Bioclastic Limestone (composed primarily of CaCO3)

Hardness: 3-4 on Mohs scale; Color: Gray matrix with white to tan shell fragments; Luster: Dull to earthy; Structure: Fragmental (bioclastic) matrix; Specific Gravity: 2.3–2.7

Hardness
3-4 on Mohs scale
Color
Gray matrix with white to tan shell fragments
Luster
Dull to earthy
Identified More sedimentary

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Physical properties

Hardness: 3-4 on Mohs scale; Color: Gray matrix with white to tan shell fragments; Luster: Dull to earthy; Structure: Fragmental (bioclastic) matrix; Specific Gravity: 2.3–2.7

Formation & geological history

Formed in high-energy marine environments (beaches or shallow reefs) where shells are broken by wave action and cemented over time by calcium carbonate. Most specimens date from the Paleozoic to Cenozoic eras.

Uses & applications

Used primarily as decorative garden stones, historical building material (especially in Florida and the Caribbean), and for educational/fossil collecting purposes.

Geological facts

Famous structures like the Castillo de San Marcos in St. Augustine, Florida, were built using coquina limestone because the 'spongy' nature of the rock absorbed cannonball impacts rather than shattering.

Field identification & locations

Identify in the field by looking for visible shell casts, molds, or whole fossils embedded in a fine-grained matrix. It will react (fizz) when exposed to a weak acid like vinegar due to the calcium carbonate content.