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Page 13, results 301 - 325

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Quaternary geology, Cold Bay and False Pass quadrangles, Alaska Peninsula
Frederic H. Wilson, Florence R. Weber
2001, Report, Geologic studies in Alaska by the U.S. Geological Survey, 1999
Recent mapping and interpretation of Quaternary geologic features has improved our understanding of the interaction between volcanic, glacial, and tectonic activity in the Cold Bay and False Pass 1:250,000-scale quadrangles on the Alaska Peninsula. The glacial and volcanic record of the map area strongly suggests that continental-shelf glaciations and two...
Mississippi Valley-type lead-zinc deposits through geological time: Implications from recent age-dating research
D. L. Leach, D. Bradley, Michael T. Lewchuk, David T. A. Symons, G. De Marsily, J. Brannon
2001, Mineralium Deposita (36) 711-740
Remarkable advances in age dating Mississippi Valley-type (MVT) lead-zinc deposits provide a new opportunity to understand how and where these deposits form in the Earth's crust. These dates are summarized and examined in a framework of global tectonics, paleogeography, fluid migration, and paleoclimate. Nineteen districts have been dated by paleomagnetic...
Delineation of groundwater recharge areas, western Cape Cod, Massachusetts
John P. Masterson, Donald A. Walter
2000, Water-Resources Investigations Report 2000-4000
The unconfined sand-and-gravel aquifer in western Cape Cod, Massachusetts, which is the sole source of water supply for the communities in the area, is recharged primarily from precipitation. The rate of recharge from precipitation is estimated to be about 26 inches per year (in/yr), or about 60 percent of the...
Sources, instream transport, and trends of nitrogen, phosphorus, and sediment in the lower Tennessee River basin, 1980-96
Anne B. Hoos, J. A. Robinson, R. A. Aycock, R.R. Knight, M. D. Woodside
2000, Water-Resources Investigations Report 99-4139
In 1997, the U.S. Geological Survey (USGS) began an assessment of the lower Tennessee River Basin as part of the National Water-Quality Assessment Program. Existing nutrient and sediment data from 1980 to 1996 were compiled, screened, and interpreted to estimate watershed inputs from nutrient sources, provide a general description...
Use of chlorine-36 to determine regional-scale aquifer dispersivity, eastern Snake River Plain aquifer, Idaho/USA
L.D. Cecil, J.A. Welhan, J.R. Green, S.K. Grape, E.R. Sudicky
2000, Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms (172) 679-687
Chlorine-36 (36Cl) derived from processed nuclear waste that was disposed at the US Department of Energy's Idaho National Engineering and Environmental Laboratory (INEEL) through a deep injection well in 1958, was detected 24-28 yr later in groundwater monitoring wells approximately 26 km downgradient from the source. Groundwater samples covering the...
Temporal variations in parameters reflecting terminal-electron-accepting processes in an aquifer contaminated with waste fuel and chlorinated solvents
Jennifer T. McGuire, Erik W. Smith, David T. Long, David W. Hyndman, Sheridan K. Haack, Michael J. Klug, Michael A. Velbel
2000, Chemical Geology (169) 471-485
A fundamental issue in aquifer biogeochemistry is the means by which solute transport, geochemical processes, and microbiological activity combine to produce spatial and temporal variations in redox zonation. In this paper, we describe the temporal variability of TEAP conditions in shallow groundwater contaminated with both waste fuel and chlorinated solvents....
Isotope evidence of paleo-El Niño-Southern Oscillation cycles in loess-paleosol record in the central United States
Hongfang Wang, L.R. Follmer, Liu J. Chao-li J.
2000, Geology (28) 771-774
The δ13C of soil carbonate in rhizoconcretions collected from a loess-paleosol sequence in the central United States indicates that growing-season C3/C4 plant ratio oscillated by 35% on a 900 ± 200 yr time scale during the late Wisconsinan glaciation. The pattern appears in phase with advance and retreat of the southern...
The statistics and kinematics of transverse sand bars on an open coast
K.M. Konicki, R.A. Holman
2000, Marine Geology (169) 69-101
Ten years (1987-1996) of time exposure video images of the nearshore region at Duck, NC were used to study transverse sand bars, bathymetric features of intermediate length scales (10-200 m) oriented oblique or perpendicular to the shoreline. These transverse sand bars extend seaward from both the shoreline (trough transverse bars)...
High-Resolution Land Use and Land Cover Mapping
Water Resources Division, U.S. Geological Survey
1999, Fact Sheet 189-99
As the Nation?s population grows, quantifying, monitoring, and managing land use becomes increasingly important. The U.S. Geological Survey (USGS) has a long heritage of leadership and innovation in land use and land cover (LULC) mapping that has been the model both nationally and internationally for over 20 years. At present,...
Modern accumulation rates and a sediment budget for the Eel shelf: a flood-dominated depositional environment
Christopher K. Sommerfield, Charles A. Nittrouer
1999, Marine Geology (154) 227-241
The northern California continental margin is periodically impacted by geologically significant storms, which have a marked influence on terrigenous sediment supply, flood deposition, and long-term accumulation of fine-grained sediment on the Eel shelf. Accumulation of Eel River muds on the adjacent shelf was investigated using 210Pb and 137Cs geochronologies, in...
Surface faulting and paleoseismic history of the 1932 Cedar Mountain earthquake area, west-central Nevada, and implications for modern tectonics of the Walker Lane
J. W. Bell, C.M. DePolo, A. R. Ramelli, A.M. Sarna-Wojcicki, C.E. Meyer
1999, Geological Society of America Bulletin (111) 791-807
The 1932 Cedar Mountain earthquake (Ms 7.2) was one of the largest historical events in the Walker Lane region of western Nevada, and it produced a complicated strike-slip rupture pattern on multiple Quaternary faults distributed through three valleys. Primary, right-lateral surface ruptures occurred on north-striking faults in Monte Cristo Valley;...
Diatom paleoecology Pass Key core 37, Everglades National Park, Florida Bay
Laura Pyle, S. R. Cooper, J.K. Huvane
1998, Open-File Report 98-522
During the 20th century, there have been large-scale anthropogenic modifications to the South Florida ecosystem. The effects of these changes on Florida Bay and its biological communities are currently of political and scientific interest. This study is part of a larger effort to reconstruct the history of environmental changes in...
Catalog of the historically active volcanoes of Alaska
T. P. Miller, R. G. McGimsey, D.H. Richter, J.R. Riehle, C.J. Nye, M. E. Yount, Julie A. Dumoulin
1998, Open-File Report 98-582
Alaska hosts within its borders over 80 major volcanic centers that have erupted during Holocene time (< 10,000 years). At least 29 of these volcanic centers (table 1) had historical eruptions and 12 additional volcanic centers may have had historical eruptions. Historical in Alaska generally means the period since 1760...
Holocene geologic and climatic history around the Gulf of Alaska
D.H. Mann, A.L. Crowell, T. D. Hamilton, B. P. Finney
1998, Arctic Anthropology (35) 112-131
Though not as dramatic as during the last Ice Age, pronounced climatic changes occurred in the northeastern Pacific over the last 10,000 years. Summers warmer and drier than today's accompanied a Hypsithermal interval between 9 and 6 ka. Subsequent Neoglaciation was marked by glacier expansion after 5-6 ka and the...
Energy resources - cornucopia or empty barrel?
P.J. McCabe
1998, American Association of Petroleum Geologists Bulletin (82) 2110-2134
Over the last 25 yr, considerable debate has continued about the future supply of fossil fuel. On one side are those who believe we are rapidly depleting resources and that the resulting shortages will have a profound impact on society. On the other side are those who see no impending...
Tectonic setting of synorogenic gold deposits of the Pacific Rim
R.J. Goldfarb, G.N. Phillips, W. J. Nokleberg
1998, Ore Geology Reviews (13) 185-218
More than 420 million oz of gold were concentrated in circum-Pacific synorogenic quartz loades mainly during two periods of continental growth, one along the Gondwanan margin in the Palaeozoic and the other in the northern Pacific basin between 170 and 50 Ma. These ores have many features in common and...
Documentation of computer program (FHB1) for assignment of transient specified-flow and specified-head boundaries in applications of the modular finite-diference ground-water flow model (MODFLOW)
Stanley A. Leake, Michael R. Lilly
1997, Open-File Report 97-571
A computer program called the Flow and Head Boundary Package (FHB1) was developed for the U.S. Geological Survey three-dimensional finite-difference modular ground-water flow model, commonly referred to as MODFLOW. FHB1 allows MODFLOW users to specify flow or head boundary conditions that vary at times other than starting and ending times...
The impacts of mobile fishing gear on seafloor habitats in the Gulf of Maine (Northwest Atlantic): implications for conservation of fish populations
Peter J. Auster, Richard J. Malatesta, Richard W. Langton, Les Watting, Page C. Valentine, Carol Lee S. Donaldson, Elizabeth W. Langton, Andrew N. Shepard, War G. Babb
1997, Reviews in Fisheries Science (4) 185-202
Fishing gear alters seafloor habitats, but the extent of these alterations, and their effects, have not been quantified extensively in the northwest Atlantic. Understanding the extent of these impacts, and their effects on populations of living marine resources, is needed to properly manage current and future levels of fishing effort...
Synthesis of the paleoclimatic record from Owens Lake core OL-92
George I. Smith, James L. Bischoff, J. Platt Bradbury
1997, Book chapter, An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California
During much of the late Quaternary, Owens Lake overflowed into one or more of four successively lower-elevation basins. Most of the water came from the high, eastern slopes of the southern Sierra Nevada, and changes in the volumes of that water reflect a dominant climatic cycle of ~100 k.y. Variations...
The history of a continent from U-Pb ages of zircons from Orinoco River sand and Sm-Nd isotopes in Orinoco basin river sediments
S.L. Goldstein, N.T. Arndt, R.F. Stallard
1997, Chemical Geology (139) 271-286
We report SHRIMP U-Pb ages of 49 zircons from a sand sample from the lower Orinoco River, Venezuela, and Nd model ages of the fine sediment load from the main river and tributaries. The U-Pb ages reflect individual magmatic or metamorphic events, the Sm-Nd model ages reflect average crustal-residence ages...
Circulation and effluent dilution modeling in Massachusetts Bay : model implementation, verification and results
Richard P. Signell, Harry L. Jenter, Alan F. Blumberg
1996, Open-File Report 96-15
A three-dimensional hydrodynamic model was developed as part of a cooperative U.S. Geological Survey/Massachusetts Water Resources Authority program to study contaminated sediment accumulation and transport in Massachusetts Bay. This report details the development of the model and assesses how well the model represents observed currents and water properties in the...
Catalog of earthquake hypocenters for Augustine, Redoubt, Iliamna, and Mount Spurr volcanoes, Alaska: January 1, 1991 - December 31, 1993
Arthur D. Jolly, John A. Power, Scott D. Stihler, Lalitha N. Rao, Gail Davidson, John F. Paskievitch, Steve Estes, John C. Lahr
1996, Open-File Report 96-70
The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska, Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained a program of seismic monitoring at potentially active volcanoes in the Cook Inlet region since 1988. The...
Hydrogeology and simulation of ground-water flow at the South Well Field, Columbus, Ohio
W. L. Cunningham, E. Scott Bair, W.P. Yost
1996, Water-Resources Investigations Report 95-4279
The City of Columbus, Ohio, operates four radial collector wells in southern Franklin County. The 'South Well Field' is completed in permeable outwash and ice-contact deposits, upon which flow the Scioto River and Big Walnut Creek. The wells are designed to yield approximately 42 million gallons per day; part of...