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Page 4602, results 115026 - 115050

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Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1982-84
Marilyn E. Pabst, Barbara J. Dague
1984, Water-Resources Investigations Report 84-4357
Continuing studies are being made in west-central Kansas to provide up-to-date information to aid in the management of ground water for irrigation.  This report, prepared in cooperation with the Western Kansas Groundwater Management District No. 1, presents the fourth in a series of studies that uses a statistical technique, called...
Stratigraphy and structure of the western Kentucky fluorspar district
R. D. Trace, D.H. Amos
1984, Professional Paper 1151-D
The western Kentucky fluorspar district is part of the larger Illinois-Kentucky fluorspar district, the largest producer of fluorspar in the United States. This report is based largely on data gathered from 1960 to 1974 during the U.S. Geological Survey-Kentucky Geological Survey cooperative geologic mapping program of Kentucky. It deals chiefly...
Map of the Carpinteria area and vicinity, Santa Barbara County, California, showing water-level contours for March 1983 and net change in water level between March 1982 and March 1983
W. R. Moyle Jr.
1984, Water-Resources Investigations Report 84-4067
A water-level contour map of the Carpinteria area, California, was constructed using 34 water-level measurements made by the Carpinteria County Water District in March 1983. Also shown on the map are five hydrographs that show water-level fluctuations in each well between 1978 and 1983. In addition, a water-level net-change map...
Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida
J.M. Berdan
1984, Professional Paper 1066-J
Leperditicopid ostracodes from the Ordovician formations of Kentucky occur in micritic to fine-grained carbonate rocks believed to represent shallow-water facies. They are found at widely separated horizons in the Middle Ordovician High Bridge Group, the Middle and Upper Ordovician Lexington Limestone, and the Upper Ordovician Ashlock, Bull Fork, and Drakes...
Hydrogeologic data from a test well at Kathryn Abbey Hanna Park, City of Jacksonville, Florida
D.P. Brown, R.A. Johnson, J.S. Baker
1984, Open-File Report 84-143
A 2,026-foot test well was drilled at Hanna Park, City of Jacksonville, Florida, to obtain hydrogeologic data. Drill cuttings and water samples were collected, and water-level measurements and lithologic and geophysical logs were made. The well is constructed with 6-inch diameter casing from land surface to a depth of 1,892...
Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado
K.L. Lindskov, B. A. Kimball
1984, Professional Paper 1307
Proposed oil-shale mining in northeastern Utah is expected to impact the water resources of a 3,000-square-mile area. This report summarizes a comprehensive hydrologic investigation of the area which resulted in 13 published reports. Hydrologic information obtained during 1974-80 was used to evaluate the availability of water and to evaluate potential...
Effects of urbanization on three ponds in Middleton, Wisconsin
Leo B. House
1984, Water-Resources Investigations Report 84-4051
A digital hydrologic model was used to simulate the effects of future residential development on pond inflow volumes and resulting water levels of three ponds in Middleton, Wisconsin. The model computed the daily water budget and the resulting water level for each pond. The results of the model calibration are...