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Hagerman Fossil Beds National Monument
Nature & Science
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| NPS Photo | | Looking south from Fossil Gulch |
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Hagerman Fossil Beds National Monument, known mostly for its fossils from the late Pliocene and Pleistocene epochs, contains one of the world’s richest known deposits of fossil horses, Equus simplicidens, thought to be a link between prehistoric and modern horses.
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, recognized as one of the six most important sites in the world regarding the fossil history of horses.
Hagerman Fossil Beds is nationally and internationally significant for its world-class paleontological resources. It includes the world’s richest fossil deposits, in quality, quantity, and diversity, from the late Pliocene epoch. Many of its fossils represent the last vestiges of species that existed before the last Ice Age, the Pleistocene, and the earliest ‘modern’ flora and fauna.
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.
The Monument is also one of three National Park system units containing a portion of the Oregon Trail National Historic Trail.
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| A Copyright Protected Jay Matternes Mural |
| An artist's view of how the Fossil Beds may have looked like during the Pliocene Epoch. |
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An artist rendition of the ecosystem when Hagerman Fossil Beds were deposited during the Pliocene Epoch. 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. The Smithsonian Institution directed fossil excavations in the early 1930's and many other museums and research institutions have conducted research here ever since.
Visit the Animals page to learn more about the variety of species that inhabited the area during the Pliocene Epoch.
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Did You Know?
The catastrophic Bonneville Flood thundered through the Hagerman Valley 15,000 years ago leaving behind enormous fields of rounded lava boulders – some as big as cars. They are called ‘melon gravel’ and can still be seen throughout the valley today.
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Last Updated: May 17, 2007 at 17:45 EST |
