Known mostly for its fossils from the Pliocene epoch Hagerman Fossil Beds National Monument contains one of the world's richest known deposits of the fossil horse Equus simplicidens.
In 1988, the Hagerman horse became Idaho's state fossil and Hagerman Fossil Beds became a national monument. The Monument contains the Hagerman Horse Quarry, a national natural landmark.Hagerman Fossil Beds is nationally and internationally significant for its world-class paleontological resources.
The Monument's paleontological resources are contained in a continuous, undisturbed stratigraphic record spanning at least 500,000 years. The fossils deposited here appear to represent an entire paleontological ecosystem with a variety of habitats such as wetland, riparian, and grassland savanna. Most of the fossils contained in the park are not obvious. There are no hikes or observation areas to see the fossils in place. A sampling of excavated fossils is displayed in the park visitor center, while the other fossils are studied under laboratory conditions not currently visible to park visitors. It is in the long term plans for the park to make the laboratory work and procedures more accessible to everyone.
The Monument is also one of four National Park system units containing a portion of the Oregon Trail National Historic Trail. Ruts from the wagons that used the Trail are visible from one of the marked lookout points inside the park grounds.
An artist rendition of the ecosystem when the Hagerman Fossil Beds were deposited during the Pliocene Epoch shows the variety of plants, animals, and geographic features of the area. A fluvial (river) and floodplain environment around the edge of ancient Lake Idaho deposited layers of sand, silt, and clay at least 600 feet thick. Layers of sediments have preserved an exquisite world class assemblage of Pliocene fossils.
Last updated: August 27, 2017