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The Niobrara River (/ ˌ n aɪ. ə ˈ b r ær ə /; Omaha–Ponca: Ní Ubthátha khe, pronounced [nĩꜜ ubɫᶞaꜜɫᶞa kʰe], literally "water spread-out horizontal-the" or "The Wide-Spreading Water") is a tributary of the Missouri River, approximately 568 miles (914 km) long, [2] running through the U.S. states of Wyoming and Nebraska. [3]
The Niobrara National Scenic River is in north-central Nebraska, United States, approximately 300 miles (480 km) northwest of Omaha. In 1991, Congress set aside 76 miles (120 km) for preservation under the management of the National Park Service with assistance from the local Niobrara Council. Several "outstandingly remarkable values" have been ...
Niobrara State Park is a public recreation area located at the confluence of the Missouri and Niobrara rivers in the northeast corner of Nebraska. [5] The state park occupies river bluffs to the west of the village of Niobrara and the Niobrara River. The park includes the Niobrara River Bridge, a decommissioned railroad bridge listed on the ...
Niobrara was founded in 1856, when a group of men headed by a Dr. Benneville Yeakel Shelly marked their claim to an area on the banks of the Missouri River.There, a fort was built to protect the early settlers from Indian attacks. [7]
Website. Agate Fossil Beds National Monument. Agate Fossil Beds National Monumentis a U.S. National Monumentnear Harrison, Nebraska. The main features of the monument are a valleyof the Niobrara Riverand the fossils found on Carnegie Hill and University Hill. The area largely consists of grass-covered plains.
Nebraska: Niobrara River. Seventy-six miles of the 568-mile Niobrara have been designated a National Scenic River, and the unique prairie scenery is certainly part of the reason. The water snakes ...
The Niobrara River is scenic, its water is clear and clean, and there are a few Class I and II rapids. Waterfalls are found in many side canyons as streams descend into the valley. In 2010, about 50,000 people floated the Niobrara River in or near the Preserve, contributing $10 million to the local economy.
Niobrara Chalk was weathered and opalized in the Valentine phase of the Ogallala Formation. The Niobrara Formation / ˌnaɪ.əˈbrærə /, also called the Niobrara Chalk, is a geologic formation in North America that was deposited between 87 and 82 million years ago during the Coniacian, Santonian, and Campanian stages of the Late Cretaceous.