Water Resources Division, U.S. Geological Survey
1983, Open-File Report 82-808
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Page 2090, results 52226 - 52250
Publication Extents
Not all publications have extents, not all extents are completely accurateJames H. Eychaner
1983, Water Supply Paper 2201
The N aquifer is the main source of water in the 5,400-square-mile Black Mesa area in the Navajo and Hopi Indian Reservations in northeastern Arizona. The N aquifer consists of the Navajo Sandstone and parts of the underlying Kayenta Formation and Wingate Sandstone of Jurassic and Triassic age. Maximum saturated...
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-575
J. W. Stewart, A. D. Duerr, Mario Fernandez Jr.
1983, Water-Resources Investigations Report 83-4180
No abstract available....
G. R. Schiner, E. C. Hayes
1983, Open-File Report 83-869
This potentiometric map highlights: the altitude at which water level would stay in tightly cased wells; wells; springs; state water management district boundaries and sub-basin boundaries. (Lantz-PTT)...
C.B. Bentley
1983, Water-Resources Investigations Report 83-4169
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-106
R. J. Gilliom
1983, Open-File Report 82-684
No abstract available....
David H. Appel
1983, Water Supply Paper 2225
The New River Gorge National River's [a 51-mile segment of the New River between Hinton and Fayette (an abandoned community), W. Va. main attraction is a combination of scenic wilderness, fishing, cultural resources, and whitewater boating. However, recreational quality, safety, and use of the river depends in part upon the...
Fernando Gómez-Gómez, Rafael Dacosta, Miguel Orona
1983, Open-File Report 83-689
K. L. Wetzel, S. A. Hoffman
1983, Open-File Report 83-940
E.W. Henrich, D.N. Daniel
1983, Open-File Report 83-933
Drainage areas were determined for more than 7,000 sites in Wisconsin's 11 major river basins, including all named streams draining 5 or more square miles, and all unnamed streams draining 10 or more square miles. Also determined are drainage areas for gaging stations, sewage-treatment plants, dams, major highway crossings, and...
J.S. Doughman
1983, Water-Resources Investigations Report 83-4006
The subfamily Diamesinae consists of the monogeneric tribes Boreoheptagnini and Parotanypini and the diverse tribe Diamesini with seven genera. These midges are prevalent in clean, cool arctic-alpine waters, but less abundant in the lowlands. Keys and descriptions herein to the known species of these nine genera may prove valuable in...
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-125
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-552
Elinor H. Handman
1983, Circular 907
References to more than 550 reports, articles, and maps are listed alphabetically by author and are indexed by subject. The subject index includes geographic-area terms. Citations from 69 series are included; series are listed separately. The publications listed report the results of U.S. Geological Survey research and field projects throughout...
J. F. Kenny, J. R. McCauley
1983, Water-Resources Investigations Report 83-4007
Disturbances resulting from intensive coal mining in the Cherry Creek basin of southeastern Kansas were investigated using color and color-infrared aerial photography in conjunction with water-quality data from simultaneously acquired samples. Imagery was used to identify the type and extent of vegetative cover on strip-mined lands and the extent and...
J. D. Hunn, L. J. Slack
1983, Water-Resources Investigations Report 83-4075
The Santa Fe River basin is a 1,384 square-mile area in north-central Florida. The principal source of water is the Floridan aquifer, a sequence of limestone beds, the upper 300 to 800 feet of which contain potable water. The western part of the basin has the greatest potential yields for...
F.J. Heimes, R. R. Luckey
1983, Water-Resources Investigations Report 83-4123
Current ground-water use is required for the High Plains Regional Aquifer-System Analysis. In response to this need, a sampling approach was developed to estimate water pumped for irrigation on the High Plains during 1980. Pumpage was computed by combining application estimates with mapped irrigated-acreage information. Irrigation application (inches of water...
J. H. Lambing
1983, Water-Resources Investigations Report 83-4224
To document and evaluate existing conditions of water quality prior to proposed coal development in east-central Montana, water-quality data were collected at 23 sites on selected streams from October 1975 through September 1981. The data were statistically summarized and regression equations were developed to define relationships between water-quality variables. Where...
R. W. Davis, Edward W. Matthews
1983, Water Supply Paper 2202
P.E. Harrold, R.L. Burrows
1983, Water-Resources Investigations Report 83-4213
Suspended-sediment and bedload-transport rates for the Tanana River near Fairbanks can be related to water discharge, and annual sediment loads can be computed using these relations. For a site at Fairbanks the annual loads in 1982 were 26.1 million metric tons of suspended sediment and 227,000 metric tons of bedload....
J.M. Childers, D.R. Kernodle
1983, Water-Resources Investigations Report 83-4027
Surface water data were collected at selected sites in the Kobuk River Basin in northwest Alaska in August 1979 and April 1980. In August 1979, frequent heavy rains caused abnormally high flows in the basin; unit runoff values, computed from discharge measurements at 25 sites, ranged from 0.08 to 12.2...
Fitzhugh T. Lee, John F. Abel
1983, Circular 876
Subsidence, a universal process that occurs in response to the voids created by extracting solids or liquids from beneath the Earth's surface, is controlled by many factors including mining methods, depth of extraction, thickness of deposit, and topography, as well as the in situ properties of the rock mass above...
R. S. Parker, J. M. Norris
1983, Water-Resources Investigations Report 83-4084
Identifying cumulative effects of coal mining on dissolved solids downstream from multipe coal-mining operations is particularly important in western basins. The problem of identifying cumulative effects is evident in the Trout Creek drainage, a tributary to the Yampa River in northwestern Colorado, where a number of mines are active and...