
sedimentary
Coquina
Biogenic Limestone (Calcite/Aragonite)
AI-generated identification · may be incorrectHardness: 2-3 (Mohs scale); Color: tan, cream, or light brown; Luster: dull to earthy; Structure: clastic/fragmental; Composition: loosely cemented shells and coral fragments; Cleavage: none (ruptures along shell boundaries); Specific Gravity: ~2.3-2.5
- Hardness
- 2-3 (Mohs scale)
- Color
- tan, cream, or light brown
- Luster
- dull to earthy
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Physical properties
Hardness: 2-3 (Mohs scale); Color: tan, cream, or light brown; Luster: dull to earthy; Structure: clastic/fragmental; Composition: loosely cemented shells and coral fragments; Cleavage: none (ruptures along shell boundaries); Specific Gravity: ~2.3-2.5
Formation & geological history
Formed in high-energy marine or lacustrine environments (beaches/reefs) where shells are broken by wave action and later cemented by calcium carbonate (calcite). Typically younger formations from the Pleistocene or Holocene epochs.
Uses & applications
Used historically as a unique building material, in road base construction, as landscaping gravel, and as a source of lime for fertilizer.
Geological facts
Famous for its use in the construction of the Castillo de San Marcos in St. Augustine, Florida; the rock's porous nature allowed it to absorb cannonball impacts rather than shattering.
Field identification & locations
Identifiable by its 'shredded wheat' appearance consisting of visible shell fragments. Found primarily along coastal regions like Florida, North Carolina, and Shark Bay, Australia. Collectors should look for soft, crumbly textures with high fossil content.
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