Tectonics and metallogenesis of Proterozoic rocks of the Reading Prong
L.C.S. Gundersen
2004, Journal of Geodynamics (37) 361-379
Detailed geologic mapping, petrography, and major and trace-element analyses of Proterozoic rocks from the Greenwood Lake Quadrangle, New York are compared with chemical analyses and stratigraphic information compiled for the entire Reading Prong. A persistent regional stratigraphy is evident in the mapped area whose geochemistry indicates protoliths consistent with a...
Probabilistic assessment of precipitation-triggered landslides using historical records of landslide occurrence, Seattle, Washington
Jeffrey A. Coe, J. A. Michael, R. A. Crovelli, William U. Savage, W.D. Nashem, W.T. Laprade
2004, Environmental & Engineering Geoscience (10) 103-122
Ninety years of historical landslide records were used as input to the Poisson and binomial probability models. Results from these models show that, for precipitation-triggered landslides, approximately 9 percent of the area of Seattle has annual exceedance probabilities of 1 percent or greater. Application of the Poisson model for estimating...
Inorganic N and P dynamics of Antarctic glacial meltwater streams as controlled by hyporheic exchange and benthic autotrophic communities
Diane M. McKnight, R.L. Runkel, C. M. Tate, J.H. Duff, D.L. Moorhead
2004, Journal of the North American Benthological Society (23) 171-188
The McMurdo Dry Valleys of South Victoria Land, Antarctica, contain numerous glacial meltwater streams that drain into lakes on the valley floors. Many of the streams have abundant perennial mats of filamentous cyanobacteria. The algal mats grow during streamflow in the austral summer and are in a dormant...
Uranium-series coral ages from the US Atlantic Coastal Plain-the "80 ka problem" revisited
J.F. Wehmiller, K. R. Simmons, H. Cheng, R. Lawrence Edwards, J. Martin-McNaughton, L.L. York, D.E. Krantz, C.-C. Shen
2004, Quaternary International (120) 3-14
Uranium series coral ages for emergent units from the passive continental margin US Atlantic Coastal Plain (ACP) suggest sea level above present levels at the end of marine oxygen isotope stage (MIS) 5, contradicting age-elevation relations based on marine isotopic or coral reef models of ice equivalent sea level. We...
Kinematic and dynamic rupture models of the November 3, 2002 Mw7.9 Denali, Alaska, earthquake
Douglas S. Dreger, D. D. Oglesby, R. Harris, N. Ratchkovski, R. Hansen
2004, Geophysical Research Letters (31)
Regional seismic waveforms, continuous and campaign-mode GPS data, and surface slip measurements were used to obtain a kinematic model of the rupture process of the November 3, 2002 Mw 7.9 Denali, Alaska, earthquake. The event initiated as a Mw 7.0 reverse slip event on the north-dipping Susitna Glacier fault with...
Use of chemical and isotopic tracers to assess nitrate contamination and ground-water age, Woodville Karst Plain, USA
B. G. Katz, A.R. Chelette, T.R. Pratt
2004, Journal of Hydrology (289) 36-61
Concerns regarding ground-water contamination in the Woodville Karst Plain have arisen due to a steady increase in nitrate-N concentrations (0.25-0.90 mg/l) during the past 30 years in Wakulla Springs, a large regional discharge point for water (9.6 m3/s) from the Upper Floridan aquifer (UFA). Multiple isotopic and chemical tracers were...
Recalculated probability of M ≥ 7 earthquakes beneath the Sea of Marmara, Turkey
T. Parsons
2004, Journal of Geophysical Research B: Solid Earth (109)
New earthquake probability calculations are made for the Sea of Marmara region and the city of Istanbul, providing a revised forecast and an evaluation of time-dependent interaction techniques. Calculations incorporate newly obtained bathymetric images of the North Anatolian fault beneath the Sea of Marmara [Le Pichon et al., 2001; Armijo...
SWICA-2 M3: Second conference on salt water intrusion in coastal aquifers: Monitoring, modeling, and management
L.E. Marin, C.I. Voss
2004, Groundwater (42) 318-322
No abstract available...
Spatial and temporal changes in microbial community structure associated with recharge-influenced chemical gradients in a contaminated aquifer
S.K. Haack, L.R. Fogarty, T.G. West, E.W. Alm, J.T. McGuire, D.T. Long, D.W. Hyndman, L.J. Forney
2004, Environmental Microbiology (6) 438-448
In a contaminated water‐table aquifer, we related microbial community structure on aquifer sediments to gradients in 24 geochemical and contaminant variables at five depths, under three recharge conditions. Community amplified ribsosomal DNA restriction analysis (ARDRA) using universal 16S rDNA primers and denaturing gradient gel electrophoresis (DGGE)...
Assessing the resolution-dependent utility of tomograms for geostatistics
F. D. Day-Lewis, J.W. Lane Jr.
2004, Geophysical Research Letters (31)
Geophysical tomograms are used increasingly as auxiliary data for geostatistical modeling of aquifer and reservoir properties. The correlation between tomographic estimates and hydrogeologic properties is commonly based on laboratory measurements, co-located measurements at boreholes, or petrophysical models. The inferred correlation is assumed uniform throughout the interwell region; however, tomographic resolution...
A post-Galileo view of Io's interior
Laszlo P. Keszthelyi, Windy L. Jaeger, Elizabeth P. Turtle, Moses P. Milazzo, Jani Radebaugh
2004, Icarus (169) 271-286
We present a self-consistent model for the interior of Io, taking the recent Galileo data into account. In this model, Io has a completely molten core, substantially molten mantle, and a very cold lithosphere. Heat from magmatic activity can mobilize volatile compounds such as SO2 in the lithosphere, and the...
Tritium hydrology of the Mississippi River basin
R. L. Michel
2004, Hydrological Processes (18) 1255-1269
In the early 1960s, the US Geological Survey began routinely analysing river water samples for tritium concentrations at locations within the Mississippi River basin. The sites included the main stem of the Mississippi River (at Luling Ferry, Louisiana), and three of its major tributaries, the Ohio River (at Markland Dam,...
Estimating V̄s(30) (or NEHRP site classes) from shallow velocity models (depths < 30 m)
David M. Boore
2004, Bulletin of the Seismological Society of America (94) 591-597
The average velocity to 30 m [V??s(30)] is a widely used parameter for classifying sites to predict their potential to amplify seismic shaking. In many cases, however, models of shallow shear-wave velocities, from which V??s(30) can be computed, do not extend to 30 m. If the data for these cases...
Determinants of reproductive costs in the long-lived Black-legged Kittiwake: A multiyear experiment
Gregory H. Golet, Joel A. Schmutz, David B. Irons, James A. Estes
2004, Ecological Monographs (74) 353-372
We studied reproductive costs of Black-legged Kittiwakes (Rissa tridactyla) in Prince William Sound, Alaska (USA) by removing entire clutches from randomly selected nests over four successive years, and then contrasting survival and fecundity of adults from manipulated and unmanipulated nests in each subsequent year. To elucidate mechanisms that lead...
Ontogenetic behavior and migration of Gulf of Mexico sturgeon, Acipenser oxyrinchus desotoi, with notes on body color and development
B. Kynard, E. Parker
2004, Environmental Biology of Fishes (70) 43-55
We observed Suwannee River Gulf sturgeon, Acipenser oxyrinchus desotoi, in the laboratory and found free embryos (first interval after hatching) hid under rocks and did not migrate. Thus, wild embryos should be at the spawning area. Larvae (first interval feeding exogenously) initiated a slow downstream migration, and some juveniles (interval...
Lateral mixing in the Mississippi River below the confluence with the Ohio River
R. E. Rathbun, C.E. Rostad
2004, Water Resources Research (40)
Lateral dispersion coefficients for two dispersants were determined for three sections of the Mississippi River below the confluence with the Ohio River. The dispersants were the specific conductance and an industrial organic compound (trimethyltriazinetrione). Three models based on the stream tube concept were used, and lateral dispersion coefficients computed from...
Exceptionally fast growth rate of <100-yr-old tufa, Big Soda Lake, Nevada: Implications for using tufa as a peleoclimate proxy
Michael R. Rosen, G.B. Arehart, M.S. Lico
2004, Geology (32) 409-412
Large tufa mounds (>3 m tall, with a basal circumference of 5 m) have been discovered on the margin of Big Soda Lake, Nevada, USA. These tufa mounds are rooted at a maximum of 4 m below the current lake surface and are actively forming from groundwater seepage, which can...
Comparison of MODIS and AVHRR 16-day normalized difference vegetation index composite data
Kevin P. Gallo, Lei Ji, Bradley C. Reed, John L. Dwyer, Jeffery C. Eidenshink
2004, Geophysical Research Letters (31)
Normalized difference vegetation index (NDVI) data derived from visible and near-infrared data acquired by the MODIS and AVHRR sensors were compared over the same time periods and a variety of land cover classes within the conterminous USA. The relationship between the AVHRR derived NDVI values and those of future sensors...
Massive collapse of volcano edifices triggered by hydrothermal pressurization
M.E. Reid
2004, Geology (32) 373-376
Catastrophic collapse of steep volcano flanks threatens lives at stratovolcanoes around the world. Although destabilizing shallow intrusion of magma into the edifice accompanies some collapses (e.g., Mount St. Helens), others have occurred without eruption of juvenile magmatic materials (e.g., Bandai). These latter collapses can be difficult to anticipate. Historic collapses...
Interpretation of concentration‐discharge patterns in acid‐neutralizing capacity during storm flow in three small, forested catchments in Shenandoah National Park, Virginia
Karen C. Rice, Jeffrey G. Chanat, George M. Hornberger, James R. Webb
2004, Water Resources Research (40)
Episodic concentration‐discharge (c‐Q) plots are a popular tool for interpreting the hydrochemical response of small, forested catchments. Application of the method involves assuming an underlying conceptual model of runoff processes and comparing observed c‐Q looping patterns with those predicted by the model. We analyzed and interpreted c‐Q plots of acid‐neutralizing capacity (ANC) for 133...
Dispersal scaling from the world's rivers
J.A. Warrick, D.A. Fong
2004, Geophysical Research Letters (31)
Although rivers provide important biogeochemical inputs to oceans, there are currently no descriptive or predictive relationships of the spatial scales of these river influences. Our combined satellite, laboratory, field and modeling results show that the coastal dispersal areas of small, mountainous rivers exhibit remarkable self-similar scaling relationships over many orders...
Timing of oil and gas generation of petroleum systems in the Southwestern Wyoming Province
L. N. R. Roberts, M. D. Lewan, T.M. Finn
2004, Mountain Geologist (41) 87-118
Burial history, thermal maturity, and timing of petroleum generation were modeled for eight key source-rock horizons at seven locations throughout the Southwestern Wyoming Province. The horizons are the bases of the Lower Permian Phosphoria Formation, the Upper Cretaceous Mowry Shale, Niobrara Formation, Baxter Shale (and equivalents), upper part of the...
Movement and population size of American shad near a low-head lock and dam
M.M. Bailey, J. Jeffery Isely, W.C. Bridges Jr.
2004, Transactions of the American Fisheries Society (133) 300-308
We investigated the population size and the proportion of the population of American shad Alosa sapidissima that passed through the New Savannah Bluff Lock and Dam, a low-head lock and dam on the Savannah River in South Carolina and Georgia. We fitted 110 American shad with radio transmitters in 2001...
Analysing the 1811-1812 New Madrid earthquakes with recent instrumentally recorded aftershocks
K. Mueller, S. E. Hough, R. Bilham
2004, Nature (429) 284-288
Although dynamic stress changes associated with the passage of seismic waves are thought to trigger earthquakes at great distances, more than 60 per cent of all aftershocks appear to be triggered by static stress changes within two rupture lengths of a mainshock. The observed distribution of aftershocks may thus be...
Shear wave velocity, seismic attenuation, and thermal structure of the continental upper mantle
I.M. Artemieva, M. Billien, J.-J. Leveque, Walter D. Mooney
2004, Geophysical Journal International (157) 607-628
Seismic velocity and attenuation anomalies in the mantle are commonly interpreted in terms of temperature variations on the basis of laboratory studies of elastic and anelastic properties of rocks. In order to evaluate the relative contributions of thermal and non-thermal effects on anomalies of attenuation of seismic shear waves, Q−1s, and...