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The earthen dam was completed by the United States Bureau of Reclamation in May 1950, impounding the Heart River. [2] The dam has a structural height of 65 feet (20 m) and is 2,275 feet (693 m) along its crest. The dam was expanded in 1981, and an auxiliary spillway with bascule gates added.
United States Bureau of Reclamation: Dam and spillways; Type of dam: Embankment earth fill: Impounds: Heart River: Height: 142 feet (43 m) Length: 1,850 feet (560 m) Dam volume: 1,140,000 cubic yards (870,000 m 3) Spillways: 1 Morning-glory type: Spillway capacity: 5,700 cfs at 1,644.4 feet msl pool elevation: Reservoir; Creates: Lake Tschida ...
Following is a list of dams and reservoirs in North Dakota.. All major dams are linked below. The National Inventory of Dams defines any "major dam" as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3).
The land near St. Anthony Falls, the birthplace of Minneapolis and a sacred site to the Indigenous people who lived there before the arrival of Europeans, is once again coming under native ...
Shadehill Dam is a dam (constructed 1951) on the Grand River in Perkins County in northwestern South Dakota in the United States, about 10 miles (16 km) south of Lemmon.The dam and its impoundment, Shadehill Reservoir, serve mainly for flood and silt control, wildlife conservation and recreation.
Mine reclamation – Restoration of land after mineral extraction; Land recycling – Reuse of abandoned buildings or sites; Soil salinity control – Controlling the problem of soil salinity; Watertable control – Use of drainage to control the groundwater level in an area; Land reclamation – Creating new land from oceans, seas, riverbeds ...
The Reclamation Service elected to construct a new rail line on the old wagon road leading north to Idaho City. The railroad would begin at the Barberton mill near the Diversion Dam and extend to through a winding canyon up to Arrowrock. Even before the dam had been approved, Reclamation began work on the rail line.
The Bureau of Reclamation details the geology of the reservoir area: The reservoir area is a gently rolling plain with a surface blanket of glacial till over-lying thin-bedded, highly jointed Pierre Shale. In this plain the James River has cut a valley 1,000 to 4,000 feet wide and 50 to 100 feet deep, which forms the reservoir.