Rock Identifier
Fossilized Shark Tooth (Fragment) (Elasmobranchii gen. et sp. indet.) — fossil
fossil

Fossilized Shark Tooth (Fragment)

Elasmobranchii gen. et sp. indet.

Hardness: 5 on Mohs scale; Color: Dark brown, black, to charcoal gray; Luster: Sub-vitreous to dull matte; Crystal Structure: Microcrystalline hydroxyapatite (mineralized tissue); Specific Gravity: ~3.0

Hardness
5 on Mohs scale
Color
Dark brown, black, to charcoal gray
Luster
Sub-vitreous to dull matte
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Physical properties

Hardness: 5 on Mohs scale; Color: Dark brown, black, to charcoal gray; Luster: Sub-vitreous to dull matte; Crystal Structure: Microcrystalline hydroxyapatite (mineralized tissue); Specific Gravity: ~3.0

Formation & geological history

Formed via permineralization where original calcium phosphate tooth structures were gradually replaced by silica, iron, and manganese minerals in anoxic marine or estuarine sedimentary layers over millions of years (typically Eocene to Pliocene epoch).

Uses & applications

Collected as geological curiosities, educational specimens, and used in wire-wrapped jewelry or crafts.

Geological facts

Shark teeth are among the most common vertebrate fossils because sharks shed thousands of teeth during their lifetimes and enameloid is highly resistant to decay. The dark color comes from taking up iron and manganese from surrounding sediments during fossilization.

Field identification & locations

Identified by its distinctive flattened, curved morphology, glossy enamel remnant surface, and high density compared to modern bone or wood fragments. Frequently found along coastal beaches and riverbeds in the southeastern US (e.g., Florida, North Carolina, Maryland).