
sedimentary
Fossil Coral
Cnidaria Anthozoa (Fossilized)
Hardness: 3-4 (Calcite based); Color: Tan, beige, or white with dark skeletal patterns; Luster: Dull to earthy; Structure: Hexagonal or colonial pore patterns; Specific Gravity: 2.6-2.7
- Hardness
- 3-4 (Calcite based)
- Color
- Tan, beige, or white with dark skeletal patterns
- Luster
- Dull to earthy
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Physical properties
Hardness: 3-4 (Calcite based); Color: Tan, beige, or white with dark skeletal patterns; Luster: Dull to earthy; Structure: Hexagonal or colonial pore patterns; Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the replacement of organic calcium carbonate skeletons by minerals (permineralization), typically during the Devonian to Jurassic periods. Found in ancient marine sedimentary beds.
Uses & applications
Used primarily for jewelry (cabochons), interior decoration, paperweights, and as educational geological specimens.
Geological facts
Many fossil corals are hundreds of millions of years old, predating the dinosaurs. Petoskey stones from Michigan are a famous variety of fossilized colonial coral.
Field identification & locations
Identify by looking for a 'honeycomb' or 'starlike' pattern on the surface that does not wash off. They are common in areas that were once prehistoric shallow seas, like the Midwest USA or parts of North Africa.
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