
sedimentary
Coquina or Fossilized Shell Fragment
Calcium Carbonate (CaCO3) / Biogenic Limestone
AI-generated identification · may be incorrectHardness: 3 (Mohs scale), Color: White to off-white, Luster: Dull to pearly, Structure: Corrugated/ridged texture from bivalve shell, Cleavage: None (conchoidal fracture when broken)
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Physical properties
Hardness: 3 (Mohs scale), Color: White to off-white, Luster: Dull to pearly, Structure: Corrugated/ridged texture from bivalve shell, Cleavage: None (conchoidal fracture when broken)
Formation & geological history
Formed by the accumulation of biochemical remains (shells) of marine organisms. Over time, these fragments undergo lithification to become sedimentary rock. This specimen appears to be a weathered fragment of a modern or Holocene-era shell.
Uses & applications
Used primarily in construction (road base), as a source of lime, in beach restoration, and as landscaping material. Historically used as a building stone (e.g., Castillo de San Marcos).
Geological facts
The word 'coquina' is Spanish for 'tiny shell.' It is a unique rock because it is porous and soft when first quarried but hardens significantly upon exposure to air. This specific fragment shows the distinctive ribbing of a scallop or similar bivalve.
Field identification & locations
Identify by its light color, ridged texture, and reaction (fizzing) when exposed to a drop of vinegar or mild acid. Commonly found along coastal beaches and in shallow marine sedimentary deposits.
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