Mineral/Fossil

Megalodon Shark Tooth (Partial Fossil)

Otodus megalodon (fossilized in Calcium Phosphate/Apatite)

AI-generated identification · may be incorrect

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

Identified April 20, 2026More mineral/fossil →

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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.