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Not all publications have extents, not all extents are completely accurate
Estimation of potential maximum biomass of trout in Wyoming streams to assist management decisions
Wayne A. Hubert, T.D. Marwitz, Kenneth G. Gerow, N.A. Binns, R.W. Wiley
1996, North American Journal of Fisheries Management (16) 821-829
Fishery managers can benefit from knowledge of the potential maximum biomass (PMB) of trout in streams when making decisions on the allocation of resources to improve fisheries. Resources are most likely to be expended on streams with high PMB and with large differences between PMB and currently measured biomass. We...
Potentiometric maps and ground-water-level data for the industrial area, northwest of Delaware City, Delaware
Colleen A. Donnelly, Kurt C. Hinaman
1996, Open-File Report 95-318
Potentiometric maps of the water-table aquifer in the spring and fall of 1993 in the industrial area northwest of Delaware City, Delaware, are presented. The maps are based on continuously recorded ground-water-level data collected at eight wells screened in the water-table aquifer from October 15, 1993 through November 8, 1994....
Geographic, geologic, and hydrologic summaries of intermontane basins of the northern Rocky Mountains, Montana
Eloise Kendy, R.E. Tresch
1996, Water-Resources Investigations Report 96-4025
This report combines a literature review with new information to provide summaries of the geography, geology, and hydrology of each of 32 intermontane basins in western Montana. The summary of each intermontane basin includes concise descriptions of topography, areal extent, altitude, climate, 1990 population, land and water use, geology, surface...
Exchangeable hydrogen explains the pH of spodosol Oa horizons
D.S. Ross, R. J. Bartlett, M.B. David, G.B. Lawrence
1996, Soil Science Society of America Journal (60) 1926-1932
The chemistry of extremely acid Oa horizons does not conform to traditional pH, Al, and base saturation relationships. Results from two separate studies of northeastern U.S. forested soils were used to investigate relationships between pH in water or dilute salt solutions and other soil characteristics. In Oa horizons with pH...
Rationale and preliminary operational plan for a high-altitude magnetic survey over the United States
T.G. Hildenbrand, R.J. Blakely, R. E. Bracken, Lynn Edwards, Doug Hardwick, W. J. Hinze, Vic Labson, Hal Malliot, Misac Nabighian, Bruno Nilsson, Jeff Phillips, J.M. Quinn, Walter Roest
1996, Open-File Report 96-276
A proposed high-altitude survey of the U.S. with an ER-2 to collect radar data offers an exciting and cost-effective opportunity to collect magnetic anomaly data. At this workshop, a group of magnetic specialists addressed this opportunity by discussing the need for high-altitude magnetic data and by formulating a preliminary operational...
Water-quality and lake-stage data for Wisconsin lakes, water year 1995
W. J. Rose
1996, Open-File Report 96-168
The U.S. Geological Survey (USGS), in cooperation with local and other agencies, collects data at selected lakes throughout Wisconsin. These data, accumulated over many years, provide a data base for developing an improved understanding of the water quality of lakes. To make these data available to interested parties outside the...
Peak-flow frequency estimates through 1994 for gaged streams in South Dakota
M.J. Burr, K.L. Korkow
1996, Open-File Report 96-202
Annual peak-flow data are listed for 250 continuous-record and crest-stage gaging stations in South Dakota. Peak-flow frequency estimates for selected recurrence intervals ranging from 2 to 500 years are given for 234 of these 250 stations. The log-Pearson Type III procedure was used to compute the frequency relations for the...
Water-resources investigations in Wisconsin
D. E. Maertz
1996, Open-File Report 96-333
PROBLEM: Surface-water information is needed for surveillance, planning, design, hazard warning, operation, and management in water-related fields such as water supply, hydroelectric power, flood control, irrigation, bridge and culvert design, wildlife management, pollution abatement, flood-plain management, and water-resources development. An appropriate data base is necessary to provide this information. OBJECTIVE: The...
Integration of orthophotographic and sidescan sonar imagery: an example from Lake Garda, Italy
Giuseppe Gentili, David C. Twichell, Bill Schwab
1996, Conference Paper, Proceedings of the International Society for Photogrammetry and Remote Sensing XVIIIth Congress, Vienna 1996
Digital orthophotos of Lake Garda basin area are available at the scale of up to 1:10,000 from a 1994 high altitude (average scale of 1:75,000) air photo coverage of Italy collected with an RC30 camera and Panatomic film. In October 1994 the lake bed was surveyed by USGS and CISIG...
Reflected seismic waves and their effect on strong shaking during the 1989 Loma Prieta, California, earthquake
Rufus D. Catchings, W.M. Kohler
1996, Bulletin of the Seismological Society of America (86) 1401-1416
Our data indicate that critical and postcritical reflections from crustal layers and the Moho produced increased shaking at discrete distances along the San Francisco Peninsula during the 1989 Loma Prieta earthquake. These reflections may have produced an increase in amplitude that is as much as 10 times greater than that...
South Florida Ecosystem Program: Quantifying freshwater discharge for coastal hydraulic control structures in eastern Dade County, Florida
Amit Kapadia, Eric D. Swain
1996, Fact Sheet 123-96
The South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of the...
South Florida Ecosystem Program; gaging flows in northeastern Florida Bay
Eduardo Patino
1996, Fact Sheet 130-96
IntroductionThe South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of the...
Mesoscale variability of the Upper Colorado River snowpack
C. #NAME? Ling, E.G. Josberger, A.S. Thorndike
1996, Hydrology Research (27) 313-322
In the mountainous regions of the Upper Colorado River Basin, snow course observations give local measurements of snow water equivalent, which can be used to estimate regional averages of snow conditions. We develop a statistical technique to estimate the mesoscale average snow accumulation, using 8 years of snow course observations....
Ground-Water Discharge to Biscayne Bay
Vicente Quinones-Aponte
1996, Fact Sheet 131-96
Introduction  The South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of...
South Florida Ecosystem Program; seepage beneath Levee 30 in northern Dade County
Roy S. Sonenshein
1996, Fact Sheet 132-96
Introduction  The South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of...
Meurigite, a new fibrous iron phosphate resembling kidwellite
W.D. Birch, A. Pring, P.G. Self, R.B. Gibbs, E. Keck, M.C. Jensen, Eugene E. Foord
1996, Mineralogical Magazine (60) 787-793
Meurigite is a new hydrated potassium iron phosphate related to kidwellite and with structural similarities to other late-stage fibrous ferric phosphate species. It has been found at four localities so far — the Santa Rita mine, New Mexico, U.S.A.; the Hagendorf-Sud pegmatite in Bavaria, Germany; granite pegmatite veins at Wycheproof,...
Presentation and evaluation of a new multi-stage parameter estimation method using advective transport observations
Evan R. Anderman, Eileen P. Poeter, Mary C. Hill
1996, Book chapter, Calibration and Reliability in Groundwater Modelling: Proceedings of the ModelCARE'96 Conference
Observations of advective groundwater transport, generally inferred from concentration measurements, have been found to help in the estimation of groundwater flow parameters. Transverse dispersion, however, can make it difficult to determine the location of the groundwater advective front directly from concentration measurements. A three-stage iterative procedure is developed to estimate...
Concentrations and loads of selected trace elements and other constituents in the Rio Grande in the vicinity of Albuquerque, New Mexico, 1994
Todd Kelly, Howard E. Taylor
1996, Open-File Report 96-126
The Pueblo of Isleta and the New Mexico Environment Department have established water-quality standards for the Rio Grande, which flows through Albuquerque, New Mexico. Trace-element concentrations historically have been greater than maximum permissible concentrations allowed by these standards. It is not known if these concentrations are due to sources from...
Trends in chloride, dissolved-solids, and nitrate concentrations in ground water, Carson Valley and Topaz Lake Areas, Douglas County, Nevada, 1959-88
C. E. Thodal
1996, Water-Resources Investigations Report 95-4254
Rapid population growth in Douglas County, an area of approximately 750 square miles in west-central Nevada, has led to concern about the present and future effects of development on ground water. This report describes the results of two nonparametric statistical procedures applied to detect trends in concentrations of chloride, dissolved...
Hydrogeology of the Quitobaquito Springs and La Abra Plain area, Organ Pipe Cactus National Monument, Arizona, and Sonora, Mexico
R. L. Carruth
1996, Water-Resources Investigations Report 95-4295
Quitobaquito Springs, in Organ Pipe Cactus National Monument near the south end of the northwestward-trending Quitobaquito Hills, are less than 0.25 mile north of the international boundary between the United States and Mexico. The National Park Service is concerned that the natural flow from Quitobaquito Springs might be reduced by...