The archaeological record in the area dates back to the Archaic Period, sometime around 3,000 to 5,000 B.C. The Archaic Period people lived along small tributary streams that flow into the Missouri Valley. Later, Woodland Period people (500 B.C. – 1,000 A.D.) lived in the area. More recent inhabitants include the Ponca, Yankton Sioux and Omaha tribes in the late 18th and 19th centuries.[5] The MinnesotaSantee Sioux arrived on the river shore in the mid-1800s and remain in the area. In 1804, while traveling up the Missouri River on their epic journey to the Pacific Ocean, Lewis and Clark participated in a Grand council with the Yankton Sioux at a site below Calumet Bluff. This significant meeting was the first meeting with a Sioux tribe on their journey upstream.[6]
In 1874, the Bon Homme Colony of Hutterites, a branch of the Mennonite movement exiled from Austria, settled on what is now the north shore of Lewis and Clark Lake. They are the first Hutterite Colony in South Dakota and the United States. The colony maintains a traditional communal way of life.[7] The lake was filled in 1957 with the completion of construction of Gavins Point Dam across the river valley.
Location
The lake is an impoundment of the Missouri River, located approximately 811.1 miles (1,305.3 km) upstream of St. Louis, Missouri where the Missouri River joins the Mississippi River. The lake is located within Cedar and Knox Counties in Nebraska and Bon Homme and Yankton Counties in South Dakota. Lake Yankton is located immediately downstream of Gavins Point Dam. The Santee Sioux Reservation is located along the southwestern shore in Knox County. The lake is located approximately 4 miles (6.4 km) west or upstream of Yankton, South Dakota.[8]
Lewis and Clark Visitor Center
The Lewis and Clark Visitor Center is located just south of Gavins Point Dam atop Calumet Bluff with views of Lewis and Clark Lake, Lake Yankton, and the Missouri River below the dam. The visitor center is open daily from Memorial Day weekend through Labor Day weekend and open weekdays during other times of the year. The visitor center interprets the history of the Missouri River Basin, including Native Americans, pioneers, the Lewis and Clark Expedition (which traveled through the area); along with local wildlife and the history of the Corps of Engineers in the area. A theater shows educational videos on the Lewis and Clark Expedition, construction of Gavins Point Dam, and the natural history of the Missouri River Region. A bookstore offers educational books, videos, and other merchandise for sale. The visitor center is known as a viewing point for the American Bald Eagle, which frequents the Missouri River below the dam, especially in winter months. The visitors center is operated and staffed by U.S. Army Corps of Engineers Park Rangers, who also give guided tours of Gavins Point Dam and the power plant.[9]
Parks and recreation
Lake Map identifying Points of Interest and Recreational Areas.View of Lewis and Clark Lake from Calumet Bluff overlook and hiking trail in Cedar County, Nebraska.View of Lewis and Clark Lake from Lewis & Clark Recreation Area along the South Dakota shore.
Lewis and Clark Lake is a very popular regional tourist destination in the upper Midwest for camping, water sports, hiking, bird watching, hunting, fishing, swimming, and biking. Average annual public visitation exceeds one-million visitors per year to the lake area.[10] Many of these recreation areas around the lake offer boat ramps, marinas, campgrounds, and day-use areas. The upper stretches of the lake are renowned for their superior waterfowl viewing and hunting opportunities along the Missouri River flyway.
There are several issues impacting recreation, wildlife, and other issues. In 2014 zebra mussels, an aquaticinvasivemussel were discovered in the lake and have infested the reservoir and the Missouri River downstream of Gavins Point Dam.[16]
Lewis and Clark Lake is significantly impacted by sedimentation and siltation issues, diminishing the overall water surface area, water storage capacity, and recreational opportunities. Sediment carried by the Missouri River and Niobrara River is slowed and trapped within the reservoir due to the dam impounding and thus slowing the natural river flow. Studies show approximately 5.1 million tons of sediment are deposited in the lake each year, which contributes to the lake's increasing size of delta area on the western portions of the lake. Approximately 60% of the sediment comes from the Nebraska Sandhills via the Niobrara River. As of 2016, approximately 30% of the lake's overall surface area has diminished due to sedimentation deposits, and some figures project by 2045 approximately 50% of the lake will be diminished due to sedimentation deposits. Presently, there is no plan or solution to remove or slow the progression of the siltation within the lake.[17]