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Page 5303, results 132551 - 132575

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Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79
Ralph O. Patt, D. Briane Adams, Dannie L. Collins
1982, Open-File Report 82-696
This report summarizes data collected by the U.S. Geological Survey for the U.S. Department of Energy, Naval Petroleum, and Oil Shale Reserves in the Parachute Creek drainage basin of western Colorado. It includes data from five surface-water gages, two automatic sediment samplers and two water-quality monitors. Instantaneous streamflow measurements were...
Hydraulic geometry of the Platte River in south-central Nebraska
T.R. Eschner
1982, Open-File Report 82-436
At-a-station hydraulic-geometry of the Platte River in south-central Nebraska is complex. The range of exponents of simple power-function relations is large, both between different reaches of the river, and among different sections within a given reach. The at-a-station exponents plot in several fields of the b-f-m diagram, suggesting that morphologic...
Hydrology of the Arbuckle Mountain area, south-central Oklahoma
Roy W. Fairchild, Ronald L. Hanson, Robert E. Davis
1982, Open-File Report 82-775
Rocks that make up the Arbuckle-Simpson aquifer crop out over about 500 square miles in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000 to 9,000 feet...
Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis
J.K. Felmlee, R. A. Cadigan
1982, Open-File Report 82-324
Multivariate statistical analyses were performed on data from 156 mineral-spring sites in nine Western States to analyze relationships among the various parameters measured in the spring waters. Correlation analysis and R-mode factor analysis indicate that three major factors affect water composition in the spring systems studied: (1) duration of water...
Water resources data, Florida, water year 1981; Volume 2A. South Florida surface water
Water Resources Division, U.S. Geological Survey
1982, Water Data Report FL-81-2A
Water resources data for the 1981 water year for south Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; water-levels and water quality of wells; and discharge and water quality of springs. Additional water data were collected at various...
Floods of October 1977 in southern Arizona and March 1978 in central Arizona
B. N. Aldridge, J.H. Eychaner
1982, Open-File Report 82-687
Major floods occurred in October 1977 and March 1978 in Arizona. As much as 14 inches of rain fell during October 6-9, 1977, over the mountains of southern Arizona and northern Mexico and caused the highest discharge since at least 1892 on the Santa Cruz River upstream from Tucson. The...
Digital model of the Bates Creek alluvial aquifer near Casper, Wyoming
K. C. Glover
1982, Water-Resources Investigations Report 82-4068
A digital model was used to simulate ground-water flow within the Bates Creek alluvial aquifer, southwest of Casper, Wyoming. Hydrologic data collected during 1977 and 1978 were used to develop the flow model under steady-state and transient conditions. Three scenarios for operating the stream-aquifer system were evaluated with the digital...
Results of hydrologic tests and water-chemistry analyses, wells H-5A, H-5B, and H-5C, at the proposed Waste Isolation Pilot Plant site, southeastern New Mexico
Kevin F. Dennehy, Jerry W. Mercer
1982, Water-Resources Investigations Report 82-19
Data were collected during hydrologic testing at wells H-5A, H-5B, and H-5C in the northeastern part of the proposed Waste Isolation Pilot Plant site in southeastern New Mexico. The three water-bearing zones tested, the Magenta and Culebra Dolomite Members of the Rustler Formation and the Rustler Formation-Salado Formation contact, yield...
Ground-water resources of the glacial outwash along the White River, Johnson and Morgan counties, Indiana
Z. C. Bailey, T.E. Imbrigiotta
1982, Water-Resources Investigations Report 82-4016
An 88-square-mile segment of the White River valley contains an unconfined sand and gravel aquifer ranging-from a featheredge zero, to 120 feet in saturated thickness. Hydraulic conductivity is 340 feet per day, and transmissivity is as much as 35,000 square feet per day. The aquifer, recharged primarily by precipitation, gains...