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Page 3748, results 93676 - 93700

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Publication Extents

Not all publications have extents, not all extents are completely accurate
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...
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...
Some facts about aftershocks to large earthquakes in California
Lucile M. Jones, Paul A. Reasenberg
1996, Open-File Report 96-266
Earthquakes occur in clusters. After one earthquake happens, we usually see others at nearby (or identical) locations. To talk about this phenomenon, seismologists coined three terms foreshock , mainshock , and aftershock. In any cluster of earthquakes, the one with the largest magnitude is called the mainshock; earthquakes that occur...
Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' x 60' quadrangle, Nevada
S.A. Minor, G. S. Vick, M. D. Carr, R. R. Wahl
1996, Open-File Report 96-262
This map database, identified as Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' X 60' quadrangle, Nevada, has been approved for release and publication by the Director of the USGS. Although this database has been subjected to rigorous review and is substantially complete, the USGS reserves...
Recharge to and discharge from the Edwards aquifer in the San Antonio area, Texas, 1995
D.S. Brown, J.T. Patton
1996, Open-File Report 96-181
The Edwards aquifer is the sole source of public water supply for more than 1 million people in the San Antonio area and supplies large quantities of water for agriculture, industry, and the military. The dissolutioned, faulted limestone aquifer is the major source of water for Bexar, Comal, Hays, Medina,...
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....
Gold placers of the historical Fortymile River region, Alaska
Warren E. Yeend
1996, Bulletin 2125
The Fortymile River region in east-central Alaska has a long and colorful history as the site of the first major gold discovery in interior Alaska. Placer gold has been mined in the region nearly every year since its original discovery in 1886. Total gold production is approximately 500,000 troy ounces....
Geology, geochemistry, and tectonostratigraphic relations of the crystalline basement beneath the coastal plain of New Jersey and contiguous areas
Richard A. Volkert, Avery Drake Jr., Peter J. Sugarman
1996, Professional Paper 1565-B
Coastal plain sediments are underlain by pre-Mesozoic crystalline rocks. The inner coastal plain is underlain by schist that is correlated with the Potomac Terrane, as well as by mafic rocks probably equivalent to the Wilmington or Bel Air-Rising Sun terranes. The northern and central outer coastal plain is underlain by...