Nestled in the foothills of the Sierra Nevada Mountains near Bakersfield is Sharktooth Hill. First documented by William P. Blake in 1853, Sharktooth Hill is one of the most significant Miocene fossil sites in the world

Sharktooth Hill is a middle Miocene marine exposure of the Round Mountain Silt unit of the Temblor Formation. Using magnetic stratigraphy data, the age of this unit is estimated to be around 15.2 and 16 million years old (Prothero et al., 2008).

However, above the bone beds, the sediments accumulated in the Temblor Sea at a fast rate, and animal remains were not disturbed by ocean currents. So, occasionally associated specimens of marine animals, such as Cetaceans, Sea Lions, Sea Cows, and Sea Turtles can be found. Examples of these associated specimens can be seen at the Beuna Vista Museum of Natural History.

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