About this property
Agate Fossil Beds National Monument is a U.S. National Monument near Harrison, Nebraska. The main features of the monument are a valley of the Niobrara River and the fossils found on Carnegie Hill and University Hill. The area largely consists of grass-covered plains. Plants on the site include prairie sandreed, blue grama, little bluestem and needle and thread grass, and the wildflowers lupin, spiderwort, western wallflower and sunflowers. Most of the land that is now the National Monument was part of the Agate Springs Ranch, a working cattle ranch, owned by James and Kate Cook, who bought the ranch in 1887. In 1892, Erwin H. Barbour of the University of Nebraska was the first scientist to examine artifacts at the site. In 1904, Olaf Peterson of the Carnegie Museum in Pittsburgh was the first paleontologist to do extensive excavations. Between 1904 and 1923 there was spirited competition between groups of paleontologists from The American Museum of Natural History, Yale University, and other institutions. The findings were especially significant because they contained full skeletons of extinct Miocene mammals, species previously only known through fragments. There are several theories as to why such a rich trove of fossils is found at this location. One is that a drought may have brought a large number of herd animals together near sparse water sources, where they died in proximity to each other. Another is that animal carcasses were swept down the ancient rivers and deposited there due to the particular geometry of the river bends and eddies. Another is that animals became trapped in quicksand there. The monument's museum collection also contains more than 500 artifacts from the Cook Collection of Plains Indians artifacts. The national monument was authorized on June 5, 1965, but was not established until June 14, 1997. The Harold J. Cook Homestead (Bone Cabin Complex) was listed on the National Register of Historic Places in 1977. Agate Fossil Beds is maintained by the National Park Service. The site is best known for a large number of well-preserved Miocene fossils, many of which were found at dig sites on Carnegie and University Hills. Fossils from the Harrison Formation and Anderson Ranch Formation, which date to the Arikareean in the North American land mammal classification, about 20 to 16.3 million years ago, are among some of the best specimens of Miocene mammals. Merychippus and Parahippus, ancestors of the modern day horse. Menoceras, pony-sized rhinoceros, the most common animal found in the fossil beds. Daphoenodon and Ysengrinia, two types of mid-sized bear dogs.
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Property data from the National Register of Historic Places, National Park Service (public domain).
Description adapted from Wikipedia under the Creative Commons Attribution-ShareAlike 4.0 International License.
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Questions about this property
When was Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation) listed on the National Register?
Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation) was listed on the National Register of Historic Places on October 30, 2013.
What type of historic resource is Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation)?
Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation) is classified as a district in the National Register of Historic Places.
What is the period of significance for Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation)?
The period of significance for Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation) is recorded as the modern era, specifically around 1997.
Can I research the history near Agate Fossil Beds National Monument (Boundary Increase and Additional Documentation)?
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