paleontology

In some places along the Caloosahatchee River, the banks are made up of river bottom deposited by the U.S. Army Corps. of Engineers' dredges. Shark teeth are the most common finds in a region is known as the Caloosahatchee Formation. The material is from the Pleistocene Epoch, which spans 10,000 to 1.8 million years.

Pleistocene shark teeth from the Caloosahatchee Formation

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One Response to “caloosahatchee_shark_teeth”

  1. joe says:

    great picture of a fossil

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