
Mineral/Fossil
Megalodon Shark Tooth (Partial Fossil)
Otodus megalodon (fossilized in Calcium Phosphate/Apatite)
Hardness: 5 (Enamel); Color: Gray, black, and tan (due to permineralization); Luster: Sub-vitreous to dull; Structure: Fossilized organic dental tissue; Cleavage: None
- Hardness
- 5 (Enamel)
- Color
- Gray, black, and tan (due to permineralization)
- Luster
- Sub-vitreous to dull
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Physical properties
Hardness: 5 (Enamel); Color: Gray, black, and tan (due to permineralization); Luster: Sub-vitreous to dull; Structure: Fossilized organic dental tissue; Cleavage: None
Formation & geological history
Formed through permineralization where minerals from surrounding sediment (often phosphate-rich) replace organic material over millions of years. This specimen likely dates to the Miocene or Pliocene epochs (approximately 23 to 3.6 million years ago).
Uses & applications
Predominantly for fossil collecting and scientific research. Highly valued as decorative display pieces and historical artifacts of ancient marine life.
Geological facts
Megalodon was the largest shark that ever lived, reaching lengths of up to 50-60 feet. Their teeth are the most common fossil remains found because sharks lose thousands of teeth throughout their lives.
Field identification & locations
Identify by the characteristic 'bourlette' (the V-shaped area between the crown and root) and serrated edges, though this specimen is heavily worn/eroded. Commonly found in coastal riverbeds and offshore deposits in the Southeastern United States, particularly Florida and South Carolina.
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