fossil

Fossil shark teeth

Likely fossilized shark teeth, possibly Carcharhiniformes or related sharks; exact species cannot be determined from the photo.

AI-generated identification · may be incorrect

Gray-brown, triangular teeth with serrated or worn margins and mineralized enamel; hardness roughly 5–7, with a glossy enamel luster and dense, noncrystalline fossil structure. The dark coloration commonly results from replacement minerals such as phosphate, silica, or iron oxides.

Identified August 9, 2026More fossil →

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At a glance

Common name: Fossil shark teeth
Scientific name: Likely fossilized shark teeth, possibly Carcharhiniformes or related sharks; exact species cannot be determined from the photo.
Category: fossil
Identified: August 9, 2026
Method: Standard

AI Estimated Value

Approximately $5–$30 each for common small specimens; $50–$500+ for large, exceptionally complete, rare, or scientifically identified teeth.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

These are biological fossils rather than rocks, formed when shark teeth were buried in marine sediment and mineralized during diagenesis, commonly over millions of years. The specimens may derive from Cenozoic marine deposits, but age cannot be established visually.

Uses & applications

Primarily used for fossil collecting, educational displays, and jewelry; value depends strongly on species, size, completeness, preservation, and provenance.

Geological facts

Sharks continuously shed teeth throughout life, so teeth are among the most abundant vertebrate fossils. Serrations and crown shape can help identify shark groups, while worn edges may reflect feeding or transport.

Field identification & locations

Identify by the enamel-covered crown, distinct root, bilateral symmetry, and cutting edges; genuine fossils usually show mineral staining and varying density. Common sources include Florida, South Carolina, Morocco, Indonesia, and Australia.