Rock Identifier
Coquina or Fossiliferous Conglomerate (Bioclastic Rudstone (variable composition)) — sedimentary
sedimentary

Coquina or Fossiliferous Conglomerate

Bioclastic Rudstone (variable composition)

Hardness: 3-7 (variable based on matrix/inclusion); Color: Brown, tan, and white; Luster: Dull/earthy matrix with pearly shell fragments; Structure: Coarse-grained, clastic; Cleavage: None (fractures around grains).

Hardness
3-7 (variable based on matrix/inclusion)
Color
Brown, tan, and white
Luster
Dull/earthy matrix with pearly shell fragments
Identified More sedimentary
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Physical properties

Hardness: 3-7 (variable based on matrix/inclusion); Color: Brown, tan, and white; Luster: Dull/earthy matrix with pearly shell fragments; Structure: Coarse-grained, clastic; Cleavage: None (fractures around grains).

Formation & geological history

Formed in high-energy marine or coastal environments where shell fragments and pebbles are rapidly buried and cemented by calcium carbonate (calcite) or iron oxide. Typical of the Holocene to Pleistocene epochs.

Uses & applications

Mostly used as a decorative landscaping stone, a collector's specimen for paleontology enthusiasts, or historically as a building material in coastal regions.

Geological facts

Famous structures like the Castillo de San Marcos in Florida were built from similar coquina rock, which was effective because its porous nature could absorb the shock of cannonballs without shattering.

Field identification & locations

Identify by looking for visible shell fragments and smooth pebbles cemented in a sandy or dark matrix. Common on beaches in Florida, the Carolinas, and along the Gulf Coast.