The Paleontology of North America

The Tertiary in Oregon, US

 map

undifferentiated rock units

See exposures in this state from the:

Quaternary
Tertiary
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Precambrian

Tertiary Fossils
Fossil photos from Tertiary in Oregon

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Paleontology and geology

During the early Tertiary, Oregon was warm and humid. Fossil turret shells, fig shells, and cockles indicate that the marine waters off the coast were warm. Rainforests grew along the coast with wet forests extending farther inland. Hyaenadonts, early cats, and other predators fed on large hoofed mammals, such as brontotheres and amynodonts. By the middle Tertiary, conditions were cooler and drier. Clams, snails, and other marine organisms similar to modern species inhabited the waters off Oregon’s coast, and forests of oak and alder covered the landscape. Horses, camels, deer, bears, weasels, dogs, and cats, as well as larger mammals like the gomphotheres (early elephants), rhinoceroses and bear-dogs wandered the landscape. Tectonic activity during the Tertiary caused the uplift of the Coast Range and the Cascades in central Oregon.

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