
sedimentary
Fossiliferous Limestone (Coquina / Shell Limestone)
Biogenic Limestone (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3-4 (Mohs scale); Color: Rusty brown, tan, and white; Luster: Dull to earthy; Structure: Accumulation of visible shell fragments (bioclasts); Specific Gravity: 2.3-2.7.
- Hardness
- 3-4 (Mohs scale)
- Color
- Rusty brown, tan, and white
- Luster
- Dull to earthy
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Physical properties
Hardness: 3-4 (Mohs scale); Color: Rusty brown, tan, and white; Luster: Dull to earthy; Structure: Accumulation of visible shell fragments (bioclasts); Specific Gravity: 2.3-2.7.
Formation & geological history
Formed in high-energy marine or coastal environments where shell debris (mollusks, brachiopods) accumulates rapidly and is cemented together by calcite. Often found in strata from the Paleozoic to Cenozoic eras.
Uses & applications
Used primarily in building construction (historically for forts and walls), as road base material, in the manufacturing of cement, or as decorative garden stones.
Geological facts
Famous structures like the Castillo de San Marcos in Florida were built from coquina; the stone's porous nature allowed it to absorb cannonball impacts rather than shattering.
Field identification & locations
Identify by a 'fizz' test (reacts with dilute hydrochloric acid) and the presence of visible, often broken shell fragments. Common in coastal regions and ancient seafloor deposits.
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