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Page 198, results 4926 - 4950

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Sedimentary basins reconnaissance using the magnetic Tilt-Depth method
A. Salem, S. Williams, E. Samson, D. Fairhead, D. Ravat, R.J. Blakely
2010, Exploration Geophysics (41) 198-209
We compute the depth to the top of magnetic basement using the Tilt-Depth method from the best available magnetic anomaly grids covering the continental USA and Australia. For the USA, the Tilt-Depth estimates were compared with sediment thicknesses based on drilling data and show a correlation of 0.86 between the...
Probabilistic seismic hazard estimates incorporating site effects - An example from Indiana, U.S.A
J.S. Hasse, C.H. Park, R.L. Nowack, J.R. Hill
2010, Environmental & Engineering Geoscience (16) 369-388
The U.S. Geological Survey (USGS) has published probabilistic earthquake hazard maps for the United States based on current knowledge of past earthquake activity and geological constraints on earthquake potential. These maps for the central and eastern United States assume standard site conditions with Swave velocities of 760 m/s in the...
Geologic map of Lassen Volcanic National Park and vicinity, California
Michael A. Clynne, L.J. Patrick Muffler
2010, Scientific Investigations Map 2899
The geologic map of Lassen Volcanic National Park (LVNP) and vicinity encompasses 1,905 km2 at the south end of the Cascade Range in Shasta, Lassen, Tehama, and Plumas Counties, northeastern California (fig. 1, sheet 3). The park includes 430 km2 of scenic volcanic features, glacially sculpted terrain, and the most...
Characterization of rock samples and mineralogical controls on leachates
Jane M. Hammarstrom, Charles A. Cravotta III, Daniel G. Galeone, John C. Jackson, Frank T. Dulong
Roger J. Hornberger, Keith B.C. Brady, editor(s)
2009, Report, Development and interpretation of the ADTI-WP2 Leaching Column Method (kinetic test procedure for the prediction of coal mine drainage quality). EPA Method 1627
Rocks associated with coal beds typically include shale, sandstone, and (or) limestone. In addition to common rock-forming minerals, all of these rock types may contain sulfide and sulfate minerals, various carbonate minerals, and organic material. These different minerals have inherently different solubility characteristics, as well as different acid-generating or acid-neutralizing...
Diffusion-equation representations of landform evolution in the simplest circumstances: Appendix C
Thomas C. Hanks
2009, Book, Friends of the Pleistocene 2009 Pacific Cell Field Trip: Paleoseismic, geomorphic, and geodetic studies across the Central Great Basin: Exploring active deformation along the eastern edge of the Pacific/North American plate boundary.
The diffusion equation is one of the three great partial differential equations of classical physics. It describes the flow or diffusion of heat in the presence of temperature gradients, fluid flow in porous media in the presence of pressure gradients, and the diffusion of molecules in the presence of chemical...
Preliminary results of the North American Soil Geochemical Landscapes Project, northeast United States and Maritime Provinces of Canada
Eric C. Grunsky, David B. Smith, Peter W.B. Friske, Laurel G. Woodruff
2009, Conference Paper, 24th International Applied Geochemistry Symposium
The results of a soil geochemical survey of the Canadian Maritime provinces and the northeast states of the United States are described. The data presented are for the <2-mm fraction of the surface layer (0-5 cm depth) and C horizons of the soil. Elemental determinations were made by ICP-MS following...
Introduction to paleoenvironments of Bear Lake, Utah and Idaho, and its catchment
Joseph G. Rosenbaum, Darrell S. Kaufman
2009, Special Paper of the Geological Society of America (450) v-xiii
In 1996 a group led by the late Kerry Kelts (University of Minnesota) and Robert Thompson (U.S. Geological Survey) acquired three piston cores (BL96-1, -2, and -3) from Bear Lake. The coring arose from their recognition of Bear Lake as a potential repository of long records of paleoenvironmental change. They...
Is the track of the Yellowstone hotspot driven by a deep mantle plume? - Review of volcanism, faulting, and uplift in light of new data
Kenneth L. Pierce, Lisa A. Morgan
2009, Journal of Volcanology and Geothermal Research (188) 1-25
Geophysical imaging of a tilted mantle plume extending at least 500 km beneath the Yellowstone caldera provides compelling support for a plume origin of the entire Yellowstone hotspot track back to its inception at 17 Ma with eruptions of flood basalts and rhyolite. The widespread volcanism, combined with a large volume of...
The United States national volcanic ash operations plan for aviation
Steven Albersheim, Marianne Guffanti
2009, Natural Hazards (51) 275-285
Volcanic-ash clouds are a known hazard to aviation, requiring that aircraft be warned away from ash-contaminated airspace. The exposure of aviation to potential hazards from volcanoes in the United States is significant. In support of existing interagency operations to detect and track volcanic-ash clouds, the United States has prepared a...
Geophysical setting of western Utah and eastern Nevada between latitudes 37°45′ and 40°N
Edward A. Mankinen, Edwin H. McKee
Bryce Tripp, Ken Krahulec, Lucy Jordan, editor(s)
2009, Book chapter, Geology and Geologic Resources and Issues of Western Utah, UGA-38
Gravity and aeromagnetic data refine the structural setting for the region of western Utah and eastern Nevada between Snake and Hamlin Valleys on the west and Tule Valley on the east. These data are used here as part of a regional analysis. An isostatic gravity map shows large areas underlain...
Simulations of cataclysmic outburst floods from Pleistocene Glacial Lake Missoula
Roger P. Denlinger, D. R. H. O’Connell
2009, Geological Society of America Bulletin (122) 678-689
Using a flow domain that we constructed from 30 m digital-elevation model data of western United States and Canada and a two-dimensional numerical model for shallow-water flow over rugged terrain, we simulated outburst floods from Pleistocene Glacial Lake Missoula. We modeled a large, but not the largest, flood, using initial...
Eocene total petroleum system — North and East of the Eocene West Side Fold Belt Assessment Unit of the San Joaquin Basin Province
Donald L. Gautier, Allegra Hosford Scheirer
2009, Professional Paper 1713-19
The North and East of Eocene West Side Fold Belt Assessment Unit (AU) of the Eocene Total Petroleum System of the San Joaquin Basin Province comprises all hydrocarbon accumulations within the geographic and stratigraphic limits of this confirmed AU. Oil and associated gas accumulations occur in Paleocene through early middle...
Stratigraphy and conodont biostratigraphy of the uppermost Carboniferous and Lower Permian from the North American Midcontinent
Darwin R. Boardman II, Bruce R. Wardlaw, Merlynd K. Nestell
2009, Kansas Geological Survey Bulletin (255)
Part A The uppermost Wabaunsee, Admire, Council Grove, and lower Chase Groups of Kansas, Oklahoma, and Nebraska are placed into three third-order depositional sequences: a Gzhelian late-highstand sequence set, a Council Grove transgressive and highstand sequence set, and a Chase transgressive sequence set. Sequences are defined by bounding maximum-exposure surfaces...
Structural development of high-temperature mylonites in the Archean Wyoming province, northwestern Madison Range, Montana
Karl S. Kellogg, David W. Mogk
2009, Rocky Mountain Geology (44) 85-102
The Crooked Creek mylonite, in the northwestern Madison Range, southwestern Montana, is defined by several curved lenses of high non-coaxial strain exposed over a 7-km-wide, northeast-trending strip. The country rocks, part of the Archean Wyoming province, are dominantly trondhjemitic to granitic orthogneiss with subordinate amphibolite, quartzite, aluminous gneiss, and sills...
Digital seismic-reflection data from western Rhode Island Sound, 1980
K. Y. McMullen, L. J. Poppe, N.K. Soderberg
2009, Open-File Report 2009-1002
During 1980, the U.S. Geological Survey (USGS) conducted a seismic-reflection survey in western Rhode Island Sound aboard the Research Vessel Neecho. Data from this survey were recorded in analog form and archived at the USGS Woods Hole Science Center's Data Library. Due to recent interest in the geology of Rhode...
Archive of digital boomer seismic reflection data collected offshore east-central Florida during USGS cruise 00FGS01, July 14-22, 2000
Janice A. Subino, Shawn V. Dadisman, Dana S. Wiese, Karynna Calderon, Daniel C. Phelps
2009, Data Series 496
In July of 2000, the U.S. Geological Survey (USGS), in cooperation with the Florida Geological Survey (FGS), conducted a geophysical survey of the Atlantic Ocean offshore Florida's east coast from Brevard County to northern Martin County. This report serves as an archive of unprocessed digital boomer seismic reflection data, trackline...
Integrated sequence stratigraphy of the postimpact sediments from the Eyreville core holes, Chesapeake Bay impact structure inner basin
James V. Browning, Kenneth G. Miller, Peter P. McLaughlin Jr., Lucy E. Edwards, Andrew A. Kulpecz, David S. Powars, Bridget S. Wade, Mark D. Feigenson, James D. Wright
2009, Special Paper of the Geological Society of America (458) 775-810
The Eyreville core holes provide the first continuously cored record of postimpact sequences from within the deepest part of the central Chesapeake Bay impact crater. We analyzed the upper Eocene to Pliocene postimpact sediments from the Eyreville A and C core holes for lithology (semiquantitative measurements of grain size and...
Petrographic and geochemical comparisons between the lower crystalline basement-derived section and the granite megablock and amphibolite megablock of the Eyreville B core, Chesapeake Bay impact structure, USA
Gabrielle N. Townsend, Roger L. Gibson, J. Wright Horton Jr., Wolf Uwe Reimold, Ralf T. Schmitt, Katerina Bartosova
2009, Special Paper of the Geological Society of America (458) 255-275
The Eyreville B core from the Chesapeake Bay impact structure, Virginia, USA, contains a lower basement-derived section (1551.19 m to 1766.32 m deep) and two megablocks of dominantly (1) amphibolite (1376.38 m to 1389.35 m deep) and (2) granite (1095.74 m to 1371.11 m deep), which are separated by an...
High-resolution seismic-reflection images across the ICDP-USGS Eyreville deep drilling site, Chesapeake Bay impact structure
David S. Powars, Rufus D. Catchings, Mark R. Goldman, Gregory S. Gohn, J. Wright Horton Jr., Lucy E. Edwards, Michael J. Rymer, Gini Gandhok
2009, Special Paper of the Geological Society of America (458) 209-233
The U.S. Geological Survey (USGS) acquired two 1.4-km-long, high-resolution (~5 m vertical resolution) seismic-reflection lines in 2006 that cross near the International Continental Scientific Drilling Program (ICDP)-USGS Eyreville deep drilling site located above the late Eocene Chesapeake Bay impact structure in Virginia, USA. Five-meter spacing of seismic sources and geophones...
Anacostia River fringe wetlands restoration project: final report for the five-year monitoring program (2003 through 2007)
Cairn C. Krafft, Richard S. Hammerschlag, Glenn R. Guntenspergen
2009, Report
The 6-hectare (ha) freshwater tidal Anacostia River Fringe Wetlands (Fringe Wetlands) were reconstructed along the mainstem of the Anacostia River in Washington, DC (Photograph 1, Figure 1) during the summer of 2003. The Fringe Wetlands consist of two separate planting cells. Fringe A, located adjacent to Lower Kingman Island, on...
Differential escape from parasites by two competing introduced crabs
April M. Blakeslee, Carolyn L. Keogh, James E. Byers, Armand M. Kuris, Kevin D. Lafferty, Mark E. Torchin
2009, Marine Ecology Progress Series (393) 83-96
Although introduced species often interact with one another in their novel communities, the role of parasites in these interactions remains less clear. We examined parasite richness and prevalence in 2 shorecrab species with different invasion histories and residency times in an introduced region where their distributions overlap broadly. On the...
Hydrology and simulation of ground-water flow in the Tooele Valley ground-water basin, Tooele County, Utah
Bernard J. Stolp, Lynette E. Brooks
2009, Scientific Investigations Report 2009-5154
Ground water is the sole source of drinking water within Tooele Valley. Transition from agriculture to residential land and water use necessitates additional understanding of water resources. The ground-water basin is conceptualized as a single interconnected hydrologic system consisting of the consolidated-rock mountains and adjoining unconsolidated basin-fill valleys. Within the...
ATM Coastal Topography-Florida 2001: Eastern Panhandle
Xan Yates, Amar Nayegandhi, John Brock, A. H. Sallenger, Jamie M. Bonisteel, Emily S. Klipp, C. Wayne Wright
2009, Data Series 431
These remotely sensed, geographically referenced elevation measurements of Lidar-derived first surface (FS) topography were produced collaboratively by the U.S. Geological Survey (USGS), Florida Integrated Science Center (FISC), St. Petersburg, FL, and the National Aeronautics and Space Administration (NASA), Wallops Flight Facility, VA. This project provides highly detailed and accurate datasets of...
Water- and Bed-Sediment Quality of Seguchie Creek and Selected Wetlands Tributary to Mille Lacs Lake in Crow Wing County, Minnesota, October 2003 to October 2006
James D. Fallon, Christine S. Yaeger
2009, Scientific Investigations Report 2009-5218
Mille Lacs Lake and its tributaries, located in east-central Minnesota, are important resources to the public. In addition, many wetlands and lakes that feed Mille Lacs Lake are of high resource quality and vulnerable to degradation. Construction of a new four-lane expansion of U.S. Highway 169 has been planned along...