Water Resources Division, U.S. Geological Survey
1986, Open-File Report 83-110
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1986, Open-File Report 86-18
Maurice A. Chaffee
1986, Miscellaneous Field Studies Map 1453-C
No abstract available. ...
J. M. Robertson, M.S. Fulp, M.D. Daggett
1986, Miscellaneous Field Studies Map 1853-A
New Mexico volcanogenic massive-sulfide occurrences, which typically contain pyrite and pyrrhotite accompanied by variable amounts of base-metal sulfides and precious metals, are found within mainly subaqueous, compositionally bimodal metavolcanic successions of Early to Middle Proterozoic age that are exposed primarily in the north-central part of the state. Host rocks include...
T.C. Michalski, D.L. Richards
1986, Open-File Report 86-289
M. W. Higgins, R. L. Atkins, T. J. Crawford, R. F. Crawford III, Rebekah Brooks, R.B. Cook
1986, Open-File Report 86-372
J. G. Vedder, D. G. Howell, Hugh McLean
1986, Open-File Report 86-637
No abstract available....
R. D. Evaldi
1986, Open-File Report 85-682
Discharge and specific conductance were measured August 13, 1985 , during low base flow of Bear Creek in the vicinity of the Y-12 Plant on the Oak Ridge Reservation, Tennessee. Discharge of Bear Creek and its tributaries measured at specific sites ranged from 0 to 1.0 cubic foot per second....
George E. Gehrels, Jason B. Saleeby
1986, Open-File Report 86-275
Southern Prince of Wales Island is underlain by stratified, intrusive, and metamorphic rocks of Cretaceous through pre-Middle Ordovician age and by surficial deposits. The region was mapped originally in reconnaissance fashion by Buddington and Chapin (1929) and subsequently by W.H. Condon and I.L. Tailleur (unpublished U.S.G.S. report, 1960) primarily with...
S. J. Deverel, S.P. Millard
1986, Open-File Report 86-538
Samples of shallow ground water that underlies much of the irrigated area in the western San Joaquin Valley of California were analyzed for various major ions and trace elements, including selenium. Concentrations of the major ions generally were similar for ground water collected in the two primary geologic zones--the alluvial...
A.E. Gartner
1986, Open-File Report 86-81
J.L. Glenn, E.A. Martin, C. A. Rice
1986, Open-File Report 86-318
Sixty-two cores ranging in length from 33 to 1002 cm were collected from the tidal Potomac system and from selected tributaries downstream from the local head-of-tides between June 1978 and July 1981. Segments from selected depths below the sediment surface have been analyzed for a variety of constituents, including lead-210,...
Inyo Ellersieck, I.L. Tailleur
1986, Open-File Report 86-158
J. C. Briggs, J.S. Feiffer
1986, Water-Resources Investigations Report 84-4367
Water quality data collected from November 1979 through September 1983 at five stream stations within Rhode Island and one in Massachusetts show that concentrations of the common constituents were low. Mean water hardness at all sites was in the ' soft ' category. Sodium concentrations were less than 20 mg/L...
R.M. Norris, Carl Johnson, L.M. Jones, L.K. Hutton
1986, Open-File Report 86-96
M. L. Garrelts
1986, Open-File Report 86-130
This report gives an overview of U.S. Geological Survey, Illinois District, Water Resources Division activities related to the water resources of the State of Illinois. The report includes sections describing District organization, programs, water conditions, data collection activities, and project summaries. Also included is a complete listing of District and...
S. L. Simpson
1986, Open-File Report 86-41
R. A. Gardner
1986, Open-File Report 86-312
Time-of-travel and reaeration data were collected between June 1983 and August 1984 for seven small streams in Alabama. Rhodamine WT was used as a tracer for all the studies and propane was used in the reaeration studies. Mean velocities through the study reaches ranged from 0.06 to 0.67 ft/sec. Computed...
M. J. Ellis
1986, Open-File Report 86-526
Data utilized in preparing an interpretive hydrogeologic report on the Dakota aquifer system in Nebraska are summarized. The study area is a 370,000 sq mi area that includes all of Kansas and Nebraska and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, and Texas. The broad objective for each Regional...
Erk Reimnitz, E. W. Kempema, P. W. Barnes
1986, Open-File Report 86-298
L. W. Lenfest
1986, Water-Resources Investigations Report 84-4040
Although surface water is the principal source of irrigation water in the Saratoga Valley, Wyoming, development of groundwater for irrigation is increasing. Most of the 30 irrigation wells in the valley are capable of producing more than 200 gallons per minute. Approximately 2,700 acre-feet of groundwater for irrigation were pumped...
M. W. Bradley
1986, Water-Resources Investigations Report 85-4304
The EPA is authorized under the Safe Drinking Water Act to protect underground sources of drinking water from contamination. However, an aquifer may be exempted from protection and used for injected wastes where the aquifer meets criteria established in the EPA 's Underground Injection Control program. The Knox Group in...
P.A. Berge, J.R. Evans, J.J. Zucca, W.M. Kohler, W. D. Mooney, P.B. Dawson, M.H. Smith
1986, Open-File Report 86-362
K. Dodd, Y. Sakss
1986, Open-File Report 86-172
No abstract available....
M. W. Bradley
1986, Water-Resources Investigations Report 85-4252
The EPA has authority under the Safe Drinking Water Act to protect underground sources of drinking water from contamination by deep well injection. An aquifer, however, may be exempted from protection and used for injected wastes where the aquifer meets criteria established in the Agency 's Underground Injection Control program....