Ashfall Fossil Beds State Historical Park

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Ashfall Fossil Beds State Historical Park is a unique paleontological site located in northeastern Nebraska. The park is famous for its remarkable concentration of fossilized skeletons of ancient animals, including rhinoceroses, camels, horses, and birds, preserved within a volcanic ash layer from a massive eruption of the Yellowstone supervolcano around 12 million years ago. The fossils are exceptionally well-preserved, and visitors can see the skeletons exactly as they were found in the field.

There are many good reasons to visit Ashfall Fossil Beds State Historical Park. It provides a rare opportunity to witness the remnants of a prehistoric ecosystem and to learn about the evolutionary history of the Great Plains. The park offers many educational and interpretive programs, including guided tours, paleontology demonstrations, and exhibits. Visitors can also try their hand at fossil excavation at the on-site Dig Site.

The main attraction of the park is the Rhino Barn, a temperature-controlled building that houses the largest concentration of complete rhinoceros skeletons in the world. Other points of interest include a fossil preparation laboratory, a visitor center, and hiking trails that offer scenic views of the surrounding countryside.

Interesting facts about Ashfall Fossil Beds State Historical Park include that the fossil layer was discovered accidentally in 1971 by a road crew digging a waterline trench, and that the site is one of the few places in the world where multiple species of ancient animals are preserved together. The park is also home to diverse plant and animal life, including prairie grasses, wildflowers, and butterflies.

The best time of year to visit Ashfall Fossil Beds State Historical Park is from May to September when the weather is mild and the park offers a full range of activities. The park is open to visitors from Wednesday through Sunday during the summer season, and on weekends only during the spring and fall. Admission fees apply.