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Page 234, results 5826 - 5850

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Using Forward Looking Infrared (FLIR) imagery to detect polar bear maternal dens: Operations manual
Geoffrey S. York, Steven C. Amstrup, Kristin S. Simac
2004, BOEM MMS 2004-062
Recent research has shown that Forward Looking Infia-Red (FLIR) imagery can detect polar bear dens despite total snow cover over their deming habitat. FLIR imagers detect a AT or difference in temperature between objects in the imager's field of view. During the Arctic winter, the groundlsnow surface is typically cold,...
Transtensional deformation in the Lake Tahoe region, California and Nevada, USA
Richard A. Schweickert, M.M. Lahren, K.D. Smith, J. F. Howle, G. Ichinose
2004, Tectonophysics (392) 303-323
Dextral transtensional deformation is occurring along the Sierra Nevada–Great Basin boundary zone (SNGBBZ) at the eastern edge of the Sierra Nevada microplate. In the Lake Tahoe region of the SNGBBZ, transtension is partitioned spatially and temporally into domains of north–south striking normal faults and transitional domains with conjugate strike-slip faults....
Mitigation of earthquake damage
George Plafker
2004, Book chapter, Meeting Challenges with Geologic Maps
The article describes the use of a geologic map to help mitigate earthquake damage along the Denali Fault where the Trans-Alaska Pipeline crosses. Geologic mapping of bedrock and unconsolidated deposits reveals a history of horizontal right-lateral slip and local vertical separations at the fault. It was determined that the eastern...
Estimates of natural ground-water discharge and characterization of water quality in Dry Valley, Washoe County, West-Central Nevada, 2002-2003
David L. Berger, Douglas K. Maurer, Thomas J. Lopes, Keith J. Halford
2004, Scientific Investigations Report 2004-5155
The Dry Valley Hydrographic Area is being considered as a potential source area for additional water supplies for the Reno-Sparks area, which is about 25 miles south of Dry Valley. Current estimates of annual ground-water recharge to Dry Valley have a considerable range. In undeveloped valleys, such as Dry Valley,...
Preliminary integrated geologic map databases for the United States: Minnesota, Wisconsin, Michigan, Illinois, and Indiana
Suzanne W. Nicholson, Connie L. Dicken, Michael P. Foose, Julie Mueller
2004, Open-File Report 2004-1355
The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research....
Hydrogeologic characterization of the Modesto Area, San Joaquin Valley, California
Karen R. Burow, Jennifer L. Shelton, Joseph A. Hevesi, Gary S. Weissmann
2004, Scientific Investigations Report 2004-5232
Hydrogeologic characterization was done to develop an understanding of the hydrogeologic setting near Modesto by maximizing the use of existing data and building on previous work in the region. A substantial amount of new lithologic and hydrologic data are available that allow a more complete and updated characterization of the...
Simulation of ground-water flow and evaluation of water-management alternatives in the Assabet River Basin, Eastern Massachusetts
Leslie A. DeSimone
2004, Scientific Investigations Report 2004-5114
Water-supply withdrawals and wastewater disposal in the Assabet River Basin in eastern Massachusetts alter the flow and water quality in the basin. Wastewater discharges and stream-flow depletion from ground-water withdrawals adversely affect water quality in the Assabet River, especially during low-flow months (late summer) and in headwater areas. Streamflow depletion...
Hydrogeology and Hydrologic Landscape Regions of Nevada
Douglas K. Maurer, Thomas J. Lopes, Rose L. Medina, J. LaRue Smith
2004, Scientific Investigations Report 2004-5131
In 1999, the U.S. Environmental Protection Agency initiated a rule to protect ground water in areas other than source-water protection areas. These other sensitive ground water areas (OSGWAs) are aquifers that are not currently but could eventually be used as a source of drinking water. The OSGWA program specifically addresses...
Hydrogeologic framework of the North Fork and surrounding areas, Long Island, New York
Christopher Schubert, Richard G. Bova, Paul E. Misut
2004, Water-Resources Investigations Report 2002-4284
Ground water on the North Fork of Long Island is the sole source of drinking water, but the supply is vulnerable to saltwater intrusion and upconing in response to heavy pumping. Information on the area's hydrogeologic framework is needed to analyze the effects of pumping and drought on ground-water levels...
Regional water table (2004) and water-level changes in the Mojave River and Morongo ground-water basins, Southwestern Mojave Desert, California
Christina L. Stamos, Julia A. Huff, Steven K. Predmore, Dennis A. Clark
2004, Scientific Investigations Report 2004-5187
The Mojave River and Morongo ground-water basins are in the southwestern part of the Mojave Desert in southern California. Ground water from these basins supplies a major part of the water requirements for the region. The continuous population growth in this area has resulted in ever-increasing demands on local ground-water...
Principal facts for gravity data collected in Wisconsin: A web site and CD-ROM for distribution of data
Stephen L. Snyder, Daniel W. Geister, David L. Daniels, C. Patrick Ervin
2004, Open-File Report 2003-157
Principal facts for 40,488 gravity stations covering the entire state of Wisconsin are presented here in digital form. This is a compilation of previously published data collected between 1948 and 1992 from numerous sources, along with over 10,000 new gravity stations collected by the USGS since 1999. Also included are...
Geochemical characterization of ground-water flow in the Santa Fe Group aquifer system, Middle Rio Grande Basin, New Mexico
Niel Plummer, Laura M. Bexfield, Scott K. Anderholm, Ward E. Sanford, Eurybiades Busenberg
2004, Water-Resources Investigations Report 2003-4131
Chemical and isotopic data were obtained from ground water and surface water throughout the Middle Rio Grande Basin (MRGB), New Mexico, and supplemented with selected data from the U.S. Geological Survey (USGS) National Water Information System (NWIS) and City of Albuquerque water-quality database in an effort to refine the conceptual...
Surface- and Ground-Water Monitoring and Mapping of Selected Features at the Blue Ridge Parkway Mt. Pisgah Campground, Haywood County, North Carolina, 2002
Douglas G. Smith
2004, Open-File Report 2004-1073
During 2002, a baseline study of hydrologic conditions was conducted, and selected features were mapped within the Mt. Pisgah campground on the Blue Ridge Parkway in Haywood County, North Carolina. Field surveys were performed by using global positioning system equipment one time (January 2002) during the study to locate hydrologic...
Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa
David A. Eash
2004, Open-File Report 2004-1250
Severe flooding occurred on June 4-5, 2002, in the Maquoketa River Basin in Delaware, Dubuque, Jackson, and Jones Counties, following thunderstorm activity over east-central Iowa. The rain gage at Cascade, Iowa, recorded a 14-hour rainfall of 6.0 inches at noon on June 4. Radar indications estimated as much as 8...
Reductive dechlorination of chlorinated ethenes under oxidation-reduction conditions and potentiometric surfaces in two trichloroethene-contaminated zones at the Double Eagle and Fourth Street Superfund sites in Oklahoma City, Oklahoma
Christopher L. Braun
2004, Scientific Investigations Report 2004-5050
The Double Eagle Refining Superfund site and the Fourth Street Abandoned Refinery Superfund site are in northeast Oklahoma City, Oklahoma, adjacent to one another. The Double Eagle facility became a Superfund site on the basis of contamination from lead and volatile organic compounds; the Fourth Street facility on the basis...
Summary of the hydrogeology of the Valley and Ridge, Blue Ridge, and Piedmont Physiographic Provinces in the eastern United States
Lindsay A. Swain, Thomas O. Mesko, Este F. Hollyday
2004, Professional Paper 1422-A
The Appalachian Valley and Piedmont Regional Aquifer-System Analysis study (1988-1993) analyzed rock types in the 142,000-square-mile study area, identified hydrogeologic terranes, determined transmissivity distributions, determined the contribution of ground water to streamflow, modeled ground-water flow, described water quality, and identified areas suitable for the potential development of municipal and industrial...
Analysis of phosphorus trends and evaluation of sampling designs in the Quinebaug River Basin, Connecticut
Elaine C. Todd Trench
2004, Scientific Investigations Report 2004-5094
A time-series analysis approach developed by the U.S. Geological Survey was used to analyze trends in total phosphorus and evaluate optimal sampling designs for future trend detection, using long-term data for two water-quality monitoring stations on the Quinebaug River in eastern Connecticut. Trend-analysis results for selected periods of record during...
Ground-water flow direction, water quality, recharge sources, and age, Great Sand Dunes National Monument, south-central Colorado
Michael G. Rupert, Niel Plummer
2004, Scientific Investigations Report 2004-5027
Great Sand Dunes National Monument is located in south-central Colorado along the eastern edge of the San Luis Valley. The Great Sand Dunes National Monument contains the tallest sand dunes in North America; some rise up to750 feet. Important ecological features of the Great Sand Dunes National Monument are palustrine...
Studying ground water under Delmarva coastal bays using electrical resistivity
Frank T. Manheim, David E. Krantz, John F. Bratton
2004, Ground Water (42) 1052-1068
Fresh ground water is widely distributed in subsurface sediments below the coastal bays of the Delmarva Peninsula (Delaware, Maryland, and Virginia). These conditions were revealed by nearly 300 km of streamer resistivity surveys, utilizing a towed multichannel cable system. Zones of high resistivity displayed by inversion modeling were confirmed by...
A bootstrap approach to computing uncertainty in inferred oil and gas reserve estimates
Emil D. Attanasi, Timothy C. Coburn
2004, Natural Resources Research (13) 45-52
This study develops confidence intervals for estimates of inferred oil and gas reserves based on bootstrap procedures. Inferred reserves are expected additions to proved reserves in previously discovered conventional oil and gas fields. Estimates of inferred reserves accounted for 65% of the total oil and 34% of the total gas...
Hydrogeology, water quality, and ecology of Anderton Branch near the Quail Hollow Landfill, Bedford County, Tennessee, 1995-99
James Farmer
2004, Scientific Investigations Report 2004-5074
The Quail Hollow Landfill, located in southeastern Bedford County on the Highland Rim overlooking the Central Basin karst region of Tennessee, is constructed on the gravelly, clay-rich residuum of the Fort Payne Formation of Mississippian age. A conceptual hydrologic model of the landfill indicated that Anderton Branch was at risk...
Geologic map of the Peach Orchard Flat quadrangle, Carbon County, Wyoming, and descriptions of new stratigraphic units in the Upper Cretaceous Lance Formation and Paleocene Fort Union Formation, eastern Greater Green River Basin, Wyoming-Colorado
J. D. Honey, R. D. Hettinger
2004, Scientific Investigations Map 2835
This report provides a geologic map of the Peach Orchard Flat 7.5-minute quadrangle, located along the eastern flank of the Washakie Basin, Wyo. Geologic formations and individual coal beds were mapped at a scale of 1:24,000; surface stratigraphic sections were measured and described; and well logs were examined to...