Conde R. Thorn, G. W. Levings, S. D. Craigg, W. L. Dam, J. M. Kernodle
1990, Hydrologic Atlas 720-B
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Page 477, results 11901 - 11925
Publication Extents
Not all publications have extents, not all extents are completely accurateC.J. Smith, G. A. Payne, L. H. Tornes
1990, Open-File Report 88-84
Water-quality and streamflow data were collected in the Coteau des Prairies region of southwestern Minnesota and eastern South Dakota from 1979- 84. Data were collected to (1) document the water-quality characteristics of streams and impoundments in the Coteau area, (2) predict the impact of proposed impoundments, (3) define the amount...
A.D. Bradfield, S. D. Porter
1990, Water-Resources Investigations Report 90-4051
The Kentucky River basin, an area of approximately 7,000 sq mi, is divided into five hydrologic units that drain parts of three physiographic regions. Data on aquatic biological resources were collected and reviewed to assess conditions in the major streams for which data were available. The North, Middle, and South...
D. G. Lord, J. L. Barringer, P.A. Johnsson, P. F. Schuster, R.L. Walker, J.E. Fairchild, B.N. Sroka, Eric Jacobsen
1990, Open-File Report 88-500
Data from a 1983-86 acidic-deposition study at McDonalds Branch basin, a small (2.35-sq-mi) forested watershed in Lebanon State Forest, New Jersey include mineralogy of soil and depositional clays; physical and chemical analyses of soils; hydrologic measurements (precipitation and throughfall amounts, stream stage and discharge, and water-table altitudes); and water quality...
William L. Dam, J. M. Kernodle, G. W. Levings, S. D. Craigg
1990, Hydrologic Atlas 720-J
Anthony Maevsky, David G. Johnson
1990, Hydrologic Atlas 716
A hydrologic study of the Westfield and Farmington River basins in Massachusetts was conducted by the U.S. Geological Survey, in cooperation with the Commonwealth of Massachusetts Department of Environmental Management, Division of Water Resources, from 1984 to 1986. The study was the final part of a statewide basin-by-basin investigations program...
Dee L. Lurry, Nancy L. Barber
1990, Water-Resources Investigations Report 89-4044
Since 1950, the U.S. Geological Survey (USGS) has estimated water use in the United States at 5-year intervals. Resulting reports tabulate water use by State and by water-resources region (major river basins) for a number of categories, such as irrigation, water supply, and industrial. In 1977, the USGS began the...
R.A. Renken, Pedro Diaz, Fernando Gómez-Gómez, Vicente Quinones-Aponte
1990, Open-File Report 90-365
R. Edward Hickman
1990, Hydrologic Atlas 717
James G. Rankl
1990, Water Supply Paper 2366
A physically based point-infiltration model was developed for computing infiltration of rainfall into soils and the resulting runoff from small basins in Wyoming. The user describes a 'design storm' in terms of average rainfall intensity and storm duration. Information required to compute runoff for the design storm by using the...
Terry W. Alexander
1990, Hydrologic Atlas 712-B
This is the second report in a series of U.S. Geological Survey Hydrologic Investigations Atlases to further supplement the National Park Service general management and development concept plan for the Ozark National Scenic Riverways (National Park Service, 1981) in southeastern Missouri (fig. 1). The technical basis on which the National...
D. J. Parliman, H.W. Young
1990, Open-File Report 90-112
Hydrologic and chemical data were collected during September through November 1989 from 90 wells and 6 springs in southern Elmore County, southwestern Idaho. These data were collected to characterize the chemical quality of water in major water-yielding zones in areas near Mountain Home and the Mountain Home Air Force Base....
D. H. Appel (compiler)
1990, Open-File Report 90-150
The U.S. Geological Survey (USGS) has been active in West Virginia since the early 1900's. During recent years, the District completed several investigations as well as initiated others. An intense effort has been made to publish interpretive reports and data on a near-current basis. As a result of this effort,...
Jeffrey D. Martin, Richard F. Duwelius, Charles G. Crawford
1990, Water Supply Paper 2368-B
Six small watersheds in west-central Indiana were selected for study of the hydrologic effects of surface coal mining and reclamation. The watersheds include mined and reclaimed, mined and unreclaimed, and unmined agricultural land uses and are each less than 3 square miles in area. Surface-water, ground-water, and meteorologic data for...
Felix Rodriguez-del-Rio, Fernando Gómez-Gómez
1990, Water-Resources Investigations Report 89-4116
No abstract available. ...
D. J. Ackerman
1990, Open-File Report 90-358
No abstract available. ...
Terry W. Alexander
1990, Hydrologic Atlas 712-A
Jeffrey L. Imes
1990, Hydrologic Atlas 711-A
An investigation of the geohydrologic system in the Ozark Plateaus province (index map and Fenneman, 1938) has been made as part of the Central Midwest Regional Aquifer System Analysis (Jorgensen and Signor, 1981), a major study of the regional aquifer system in parts of 10 States. The study is one...
K.E. Goddard, editor(s)
1990, Open-File Report 89-580
The Cheyenne River System in western South Dakota has been impacted by the discharge of about 100 million metric tons of gold-mill tailings to Whitewood Creek near Lead, South Dakota. In April 1985, the U.S. Geological Survey initiated an extensive series of research studies to investigate the magnitude of the...
Jeffrey L. Imes, Brenda J. Smith
1990, Hydrologic Atlas 711-I
B. H. Ringen, P. B. Daddow
1990, Water-Resources Investigations Report 89-4002
The potential for developing water supplies from the alluvium along the Powder River between Sussex, Wyoming, and Moorehead, Montana, is very limited. The areal extent and saturated thickness of the alluvium are not large. Water in the alluvium primarily is derived from seepage from the river, which goes dry periodically....
Lowell F. W. Duell Jr.
1990, Water Supply Paper 2370-E
In Owens Valley, evapotranspiration (ET) is one of the largest components of outflow in the hydrologic budget and the least understood. ET estimates for December 1983 through October 1985 were made for seven representative locations selected on the basis of geohydrology and the characteristics of phreatophytic alkaline scrub and meadow...
Gerald L. Rockwell
1990, Open-File Report 90-177
Honey Lake Valley straddles the state line of California and Nevada, about 35 miles north of Reno; about three-fourths of the area is in California. In this report, Honey Lake Valley (also referred to as the "basin") includes the entire area within the hydrographic boundary (fig. 1). Susanville, Calif., in...
Jeffrey L. Imes, Jerri V. Davis
1990, Hydrologic Atlas 711-J
The St. Francois aquifer, the lowermost of three regional aquifers that form part of the Ozark Plateaus aquifer system, is composed of water-bearing sandstone and dolostone of Late Cambrian age. The aquifer was studied as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA, Jorgensen and Signor, 1981), a study...
J. S. Downey
1990, Water-Resources Investigations Report 90-4022
The Fairbanks-North Star Borough, Alaska, landfill is located on silt, sand, and gravel deposits of the Tanana River flood plain, about 3 miles south of the city of Fairbanks water supply wells. The landfill has been in operation for about 25 years in this sub-arctic region of discontinuous permafrost. The...