Rock Identifier
Fossilized Shark Tooth (Fragment) in Matrix (Elasmobranchii (subclass)) — fossil
fossil

Fossilized Shark Tooth (Fragment) in Matrix

Elasmobranchii (subclass)

Color: Off-white to tan matrix with an ivory-colored tooth fragment. Hardness: Tooth (5 on Mohs scale), Matrix (varies, usually 3-4). Luster: Dull/earthy matrix with slightly vitreous tooth enamel. Structure: Biological apatite replaced by minerals.

Hardness
Tooth (5 on Mohs scale), Matrix (varies, usually 3-4)
Color
Off-white to tan matrix with an ivory-colored tooth fragment
Luster
Dull/earthy matrix with slightly vitreous tooth enamel
Identified More fossil
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Physical properties

Color: Off-white to tan matrix with an ivory-colored tooth fragment. Hardness: Tooth (5 on Mohs scale), Matrix (varies, usually 3-4). Luster: Dull/earthy matrix with slightly vitreous tooth enamel. Structure: Biological apatite replaced by minerals.

Formation & geological history

Formed through permineralization in marine sedimentary environments. Thousands of shark teeth are shed over a shark's lifetime and settle in ocean floor silt, eventually fossilizing over millions of years (likely Cenozoic or Cretaceous).

Uses & applications

Educational specimens, hobbyist collecting, and small-scale jewelry components.

Geological facts

Sharks do not have bones; their skeletons are cartilage, which rarely fossilizes. The teeth are often the only part of the shark that survives as a fossil due to their high mineral content.

Field identification & locations

Identified by the distinct contrast between the smooth, pointed tooth enamel and the grainy surrounding sedimentary matrix. Found in coastal regions, riverbeds, and limestone quarries globally.