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Filter Total Items: 669

Hydrologic effects of withdrawal of ground water on the West Fargo aquifer system, eastern Cass County, North Dakota Hydrologic effects of withdrawal of ground water on the West Fargo aquifer system, eastern Cass County, North Dakota

The West Fargo area is underlain by glaciofluvial deposits, which comprise the West Fargo aquifer system* These deposits range in thickness from 5 to 227 feet. The West Fargo aquifer system extends from the vicinity of Argusville, Cass County, to at least as far south as Richland County. The aquifer system primarily consists of three aquifers, namely the West Fargo North aquifer, the...
Authors
C. A. Armstrong

Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota

High water levels of Devils Lake, North Dakota, and other terminal lakes, have, in recent years, threatened highways, agricultural land, recreational cabins, and communities located near these lakes. This study was undertaken to describe the hydrology of the Devils Lake basin and to determine how to estimate future water level probabilities. Analysis of the available hydrologic and...
Authors
Gregg J. Wiche

National water summary 1984: Hydrologic events, selected water-quality trends, and ground-water resources National water summary 1984: Hydrologic events, selected water-quality trends, and ground-water resources

Water year 1984 was a year of extreme hydrologic conditions. For the third consecutive year, precipitation and resulting runoff were well above long-term averages in most of the Nation and as much as 400 percent above average in the Southwest. National flood damages during the year were the third highest in a 10-year period (1975-84) an estimated $3.5 to $4 billion. In many of the larger...
Authors

Supplement to inventory and analyses of information for flood plain management in North Dakota Supplement to inventory and analyses of information for flood plain management in North Dakota

Governmental units that have been identified as having flood hazard areas but do not have detailed base flood information are required to use the ' best available data ' to regulate new development or expansion of existing development in flood prone areas. Information for flood plain management has been identified for 31 governmental units in North Dakota and includes the determination...
Authors
D. G. Emerson, J. D. Wald

Geohydrologic reconnaissance of the Avoca lignite deposit area near Williston, northwestern North Dakota Geohydrologic reconnaissance of the Avoca lignite deposit area near Williston, northwestern North Dakota

The Avoca lignite deposit in the Sentinel Butte Member of the Fort Union Formation consists of four potentially strippable lignite beds. Average bed thicknesses, in descending order, are 5, 5, 9, and 8 .feet. In the area between Stony Creek and Crazy Man Coulee, the lignite beds are unsaturated, and between Stony Creek and Little Muddy River, only the two lowest beds are saturated...
Authors
W.F. Horak, O.A. Crosby

Data uses and funding of the streamflow-gaging program in North Dakota Data uses and funding of the streamflow-gaging program in North Dakota

This report documents the uses, funding, and availability of the streamflow data currently collected in North Dakota. Presently (1984), 94 streamflow-gag ing stations are operated in North Dakota on a budget of $663,000. Station type, data uses, and funding sources are identified for each of the 94 stations. Data from all stations have multiple uses. All stations have sufficient...
Authors
Gerald L. Ryan

The geohydrologic system and probable effects of mining in the Sand Creek-Hanks lignite area, western Williams County, North Dakota The geohydrologic system and probable effects of mining in the Sand Creek-Hanks lignite area, western Williams County, North Dakota

The investigation was undertaken to define the geohydrology of the Sand Creek-Hanks area and to project probable hydrologic effects of lignite mining on the area. Aquifers occur in sandstone beds in the Fox Hills Sandstone and the Hell Creek Formation of Cretaceous age and in sandstone lenses and lignite beds in the Tongue River and Sentinel Butte Members of the Fort Union Formation of...
Authors
C. A. Armstrong

Small-area snow surveys on the northern plains of North Dakota Small-area snow surveys on the northern plains of North Dakota

Snow-cover data are needed for many facets of hydrology. The variation in snow cover over small areas is the focus of this study. The feasibility of using aerial surveys to obtain information on the snow water equivalent of the snow cover in order to minimize the necessity of labor intensive ground snow surveys was- evaluated. A low-flying aircraft was used to measure attenuations of...
Authors
Douglas G. Emerson, T.R. Carroll, Harold Steppuhn

National water summary 1983: Hydrologic events and issues National water summary 1983: Hydrologic events and issues

The United States as a Nation possesses abundant water resources and has developed and used those resources extensively. The national renewable supply of water is about 1,400 billion gallons per day (for the conterminous 48 States). Approximately 380 billion gallons per day of freshwater is withdrawn for use by the Nation's homes, farms, and industries, and about 280 billion gallons per...
Authors
Water Resources Division U.S. Geological Survey
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