W. A. Harenberg, M.L. Jones, I. O'Dell, S.C. Cordes
1989, Water Data Report ID-88-1
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Page 4556, results 113876 - 113900
Publication Extents
Not all publications have extents, not all extents are completely accurateT.D. Light, H. D. King, S. J. Sutley
1989, Miscellaneous Field Studies Map 2058-C
H.E. Malde
1989, Miscellaneous Field Studies Map 2063-A
Stuart W. McKenzie, David A. Curtiss
1989, Open-File Report 89-60
H. C. Mattraw Jr., William G. Wilber, William M. Alley
1989, Open-File Report 88-726
John H. Bullock Jr., Helen A. Whitney
1989, Open-File Report 89-215
D. P. Cox, T.D. Light, Bea Csejtey, D. L. Campbell, Warren Yeend
1989, Miscellaneous Field Studies Map 2058-A
M. D. Krohn
1989, Open-File Report 89-637
K. M. Kostelnik, R.R. Durlin
1989, Open-File Report 89-247
Streamflow and water quality data were collected throughout the Little Clearfield Creek basin, Clearfield County, Pennsylvania, from December 1987 through November 1988, to determine the existing quality of surface water over a range of hydrologic conditions. This data will assist the Pennsylvania Department of Environmental Resources during its review of...
W.R. Krug, W.A. Gebert, D.J. Graczyk
1989, Open-File Report 87-535
Average annual runoff was computed or estimated for 2,148 hydrologic cataloging units in the United States and Puerto Rico , for the period 1951-80. Runoff was computed from the recorded streamflow at 5,951 U.S. Geological Survey gaging stations. The runoff at more than 3,000 of these stations was estimated by...
George R. Kish, Julia L. Barringer, Randy L. Ulery
1989, Water-Resources Investigations Report 87-4181
Corrosive groundwater, which has been linked to trace-metal leaching from plumbing materials in Europe and the United States , has been identified in the Coastal Plain of New Jersey. The corrosiveness of groundwater in the Kirkwood-Cohansey aquifer system in New Jersey has been estimated by calculating values for the Aggressive...
National Earthquake Information Center
1989, Open-File Report 88-600-A
National Earthquake Information Center
1989, Open-File Report 88-600-B
Martin G. Miller, R. J. Weldon
1989, Open-File Report 89-189
No abstract available....
W.J. Haire, C. Lietz
1989, Water Data Report FL-88-2B
Water resources data for the 1988 water year in Florida consists of continuous or daily discharge for 338 streams, periodic discharge for 34 streams, miscellaneous discharge for 28 streams, continuous or daily stage for 152 streams, periodic stage for 29 streams, peak discharge for 71 streams, continuous daily tide stage...
National Earthquake Information Center
1989, Open-File Report 88-600-C
Robert E. Bracken, R. J. Horton, D. H. Rohret, R. W. Krizman, C. R. Thompson, R. A. Sneddon, H. A. Pierce, C. M. Mitchell
1989, Open-File Report 89-452
No abstract available....
K.T. Gunard, J.H. Hess, J.L. Zirbel, C.E. Cornelius
1989, Water Data Report MN-87-1
Timothy D. Liebermann, David K. Mueller, James E. Kircher, Anne F. Choquette
1989, Water Supply Paper 2358
Annual and monthly concentrations and loads of dissolved solids and major constituents were estimated for 70 streamflow-gaging stations in the Upper Colorado River Basin. Trends in streamflow, dissolved-solids concentrations, and dissolved-solids loads were identified. Nonparametric trend-analysis techniques were used to determine step trends resulting from human activities upstream and long-term...
Michael L. Jones, Annette M. Tungate
1989, Open-File Report 89-232
Hydrographs of water levels in 515 observation wells in the statewide monitoring network for the period 1982-88 are compiled for convenient use. The monitoring network is operated by the U.S. Geological Survey in cooperation with the Idaho Department of Water Resources, U.S. Bureau of Reclamation, and other Federal and State...
A. W. Coen III
1989, Water-Resources Investigations Report 89-4020
This report presents the results of a county-wide ground-water appraisal of Williams County, a mostly agricultural county of more than 36,000 people that is undergoing gradual commercial and industrial development. Most of the County's ground water is in the 80-to 320-foot thick cap of unconsolidated glacial sediments. The underlying Mississippian...
J.C. Antweiler, J. D. Love, H.J. Prostka, D. M. Kulik, L. A. Anderson, F. E. Williams, J. E. Jinks, T.D. Light
1989, Bulletin 1781
M. G. Best, D.M. Lemmon, H. T. Morris
1989, IMAP 1904
Y.E. Stoker, S.E. Henderson, B. F. McPherson
1989, Water-Resources Investigations Report 88-4162
The tidal reach of the Peace River in southwestern Florida extends about 26 miles upstream from Charlotte Harbor and is characterized by flow-direction reversals, low velocities, and salinity gradients that vary with freshwater inflow, tides, and wind. Flow reversals generally occur on each tide throughout most of the tidal reach,...
V.E. Stricklin
1989, Water-Resources Investigations Report 88-4120
This report delineates and describes the geohydrology and the susceptibility to contamination of the major aquifers in Area 3--Cullman, Fayette, Lamar, Marion, Walker, and Winston Counties , Alabama. The major aquifers in the study area are the Tuscaloosa, Pottsville, and Bangor aquifers. The Pottsville aquifer is the most extensively used...