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Filter Total Items: 673

Test drilling at Soldier Creek, Rosebud Indian Reservation, Todd County, South Dakota Test drilling at Soldier Creek, Rosebud Indian Reservation, Todd County, South Dakota

Thirty-six test holes were augered by the U.S. Geological Survey in the vicinity of Sol,,r Creek, Rosebud Indian Reservation, Todd County, South Dakota. Wells prcducing more than S gallons per minute (0.32 litre per second) from the Tertiary deposits are rare. However, as much as 20 feet (6.1 metres) of permeable alluvial deposits were penetrated in several test holes. One test ell was...
Authors
D. G. Adolphson

Geology of Griggs and Steele Counties Geology of Griggs and Steele Counties

Griggs and Steele Counties, located at the eastern edge of the Williston basin, are underlain by 400 to 2,600 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The Cretaceous Greenhorn, Carlile, Niobrara, and Pierre Formations lie directly beneath the glacial drift, and shale of the Pierre Formation is exposed in several places along the Sheyenne River. The Pleistocene...
Authors
John P. Bluemle

Delineation of buried glacial drift aquifers Delineation of buried glacial drift aquifers

Locating and delineating buried glacial-drift aquifers poses one of the major problems to hydrogeologists working in glacial terrain. To show the vertical and horizontal boundaries of aquifers, most techniques require a multiple set of maps, a fence diagram, or a combination of maps and sections. Calculations of the first two moments, mean and standard deviation, of a discontinuous...
Authors
Thomas C. Winter

Magnitude and frequency of floods in small drainage basins in North Dakota Magnitude and frequency of floods in small drainage basins in North Dakota

This report describes methods for estimating flood-peak discharges having 2- to 50-year recurrence intervals on North Dakota streams draining less than 100 square miles ( 259 square kilometres). For gaged sites, frequency estimates are provided directly. For ungaged sites, flood peaks are estimated from multiple-regression equations using drainage-area size and, in two regions, soil...
Authors
Orlo A. Crosby

Results of aquifer testing in the Belcourt area, Rolette County, North Dakota Results of aquifer testing in the Belcourt area, Rolette County, North Dakota

The city of Belcourt, Agency headquarters for the Turtle Mountain Indian Reservation, is located in northeastern Rolette County, north-central North Dakota. At the request of the U.S. Public Health Service, the U.S. Geological Survey conducted a study in the vicinity of Belcourt to assist in location of a suitable water supply for the city.
Authors
P.G. Randich, G.E. Ghering

Ground-water availability in the Belcourt area, Rolette County, North Dakota Ground-water availability in the Belcourt area, Rolette County, North Dakota

Test drilling and geologic data indicate that there are two potential aquifers in the Belcourt, N. Dak. area capable of supplying a sufficient quantity of ground water for the city of Belcourt. The Fox Hills aquifer, located about 3 miles (4.8 kilometres) west of Belcourt, could yield a sufficient quantity, as much as 500,000 gallons per day (1,900 cubic metres per day), of ground water...
Authors
P.G. Randich

Data summary of June-July 1975 floods in eastern North Dakota and northwestern Minnesota Data summary of June-July 1975 floods in eastern North Dakota and northwestern Minnesota

Torrential rains during late June and early July 1975, combined with wet antecedent conditions, caused severe flooding, mainly along the lower reaches of the Sheyenne and Maple Rivers and their tributaries in North Dakota, and in the Buffalo and Wild Rice River basins in Minnesota. The Red River of the North from the Fargo-Moorhead area to the Halstad, Minnesota area was also severely...
Authors
K.L. Lindskov

The Black Hills-Rapid City flood of June 9-10, 1972: A description of the storm and flood The Black Hills-Rapid City flood of June 9-10, 1972: A description of the storm and flood

On June 9, 1972, an almost stationary group of thunderstorms formed over the eastern Black Hills of South Dakota near Rapid City and produced record amounts of rainfall and flood discharges. Nearly 15 inches of rain fell in about 6 hours near Nemo, S. Dak., and more than 10 inches of rain fell over a 60-square-mile area. The resulting floods were the highest ever recorded in South Dakota...
Authors
Francis K. Schwarz, L.A. Hughes, E.M. Hansen, M.S. Petersen, Donovan B. Kelly

The National Stream Quality Accounting Network (NASQAN) - Some questions and answers The National Stream Quality Accounting Network (NASQAN) - Some questions and answers

One of the major new efforts of the U.S. Geological Survey is the National Stream Quality Accounting Network (NASQAN). This circular is intended to answer some of the frequently asked questions concerning concepts used in establishing NASQAN, its purposes, design, value, and future plans.
Authors
John F. Ficke, Richard O. Hawkinson

An investigation of basin effects on flood discharges in North Dakota An investigation of basin effects on flood discharges in North Dakota

An investigation of the relationship of peak discharge to causative storm variables and drainage-basin characteristics was made to provide guidelines for future analyses of frequency and magnitudes of floods from small drainage areas. The procedure used was (l) to estimate peak discharges on the ll study basins from multiple-regression models developed from the storm variables and (2) to...
Authors
Orlo A. Crosby

Geohydrology of Crow Creek and Lower Brule Indian Reservations, South Dakota Geohydrology of Crow Creek and Lower Brule Indian Reservations, South Dakota

Effective improvement of economic and social conditions of Indians living on Crow Creek and Lower Brule Reservations has been hampered by lack of adequate and reliable information about the quantity and quality of water supplies available for development. Compounding the problem, and making especially pressing the need for discovery and development of new water supplies, is the recent...
Authors
Lewis W. Howells
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