Place vs. time and vegetational persistence: A comparison of four tropical mires from the Illinois Basin during the height of the Pennsylvanian Ice Age
William A. DiMichele, T.L. Phillips, W. John Nelson
2002, International Journal of Coal Geology (50) 43-72
Coal balls were collected from four coal beds in the southeastern part of the Illinois Basin. Collections were made from the Springfield, Herrin, and Baker coals in western Kentucky, and from the Danville Coal in southwestern Indiana. These four coal beds are among the principal mineable coals of the Illinois...
Geochemical evidence for diversity of dust sources in the southwestern United States
M.C. Reheis, J. R. Budahn, P. J. Lamothe
2002, Geochimica et Cosmochimica Acta (66) 1569-1587
Several potential dust sources, including generic sources of sparsely vegetated alluvium, playa deposits, and anthropogenic emissions, as well as the area around Owens Lake, California, affect the composition of modern dust in the southwestern United States. A comparison of geochemical analyses of modern and old (a few thousand years) dust...
Influence of fracture anisotropy on ground water ages and chemistry, Valley and Ridge province, Pennsylvania
W.C. Burton, Niel Plummer, E. Busenberg, B.D. Lindsey, W.J. Gburek
2002, Ground Water (40) 242-257
Model ground water ages based on chlorofluorocarbons (CFCs) and tritium/helium-3 (3H/3He) data were obtained from two arrays of nested piezometers located on the north limb of an anticline in fractured sedimentary rocks in the Valley and Ridge geologic province of Pennsylvania. The fracture geometry of the gently east plunging fold...
Strain accumulation and rotation in western Nevada, 1993-2000
J. L. Svarc, J.C. Savage, W.H. Prescott, A. R. Ramelli
2002, Journal of Geophysical Research B: Solid Earth (107) ETG 2-1-ETG 2-11
The positions of 44 GPS monuments in an array extending from the Sierra Nevada at the latitude of Reno to near Austin, Nevada, have been measured several times in the 1993–2000 interval. The western half of the array spans the Walker Lane belt, whereas the eastern half spans the central...
Subsurface geometry and evolution of the Seattle fault zone and the Seattle Basin, Washington
Uri S. ten Brink, P.C. Molzer, M. A. Fisher, R.J. Blakely, R.C. Bucknam, T. Parsons, R. S. Crosson, K. C. Creager
2002, Bulletin of the Seismological Society of America (92) 1737-1753
The Seattle fault, a large, seismically active, east-west-striking fault zone under Seattle, is the best-studied fault within the tectonically active Puget Lowland in western Washington, yet its subsurface geometry and evolution are not well constrained. We combine several analysis and modeling approaches to study the fault geometry and evolution, including...
Trends in late Maastrichtian calcareous nannofossil distribution patterns, Western North Atlantic margin
Self-Trail J.M.
2002, Micropaleontology (48) 31-52
First and last occurrences of several Maastrichtian calcareous nannofossil species are shown to be diachronous across paleodepth and paleoenvironment using the graphic correlation method. Calcareous nannofossil assemblages examined from eleven cores from a deep- to shallow-water transect along the eastern United States Atlantic margin document that the first occurrence of...
Nitrate in aquifers beneath agricultural systems
M. R. Burkart, J.D. Stoner
2002, Conference Paper, Water Science and Technology
Research from several regions of the world provides spatially anecdotal evidence to hypothesize which hydrologic and agricultural factors contribute to groundwater vulnerability to nitrate contamination. Analysis of nationally consistent measurements from the U.S. Geological Survey's NAWOA program confirms these hypotheses for a substantial range of agricultural systems. Shallow unconfined aquifers...
Geochemistry of Mesozoic plutons, southern Death Valley region, California: Insights into the origin of Cordilleran interior magmatism
O.T. Ramo, J.P. Calzia, P.J. Kosunen
2002, Contributions to Mineralogy and Petrology (143) 416-437
Mesozoic granitoid plutons in the southern Death Valley region of southeastern California reveal substantial compositional and isotopic diversity for Mesozoic magmatism in the southwestern US Cordillera. Jurassic plutons of the region are mainly calc-alkaline mafic granodiorites with εNdi of –5 to –16, 87Sr/86Sr i of 0.707–0.726, and 206Pb/204Pb i of 17.5–20.0. Cretaceous granitoids of the region are...
Effects of colony relocation on diet and productivity of Caspian terns
Daniel D. Roby, Ken Collis, Donald E. Lyons, D. P. Craig, Jessica Y. Adkins, Anne Mary Myers, Robert M. Suryan
2002, Journal of Wildlife Management (66) 662-673
We investigated the efficacy of management to reduce the impact of Caspian tern (Sterna caspia) predation on survival of juvenile salmonids (Oncorhynchus spp.) in the Columbia River estuary. Resource managers sought to relocate approximately 9,000 pairs of terns nesting on Rice Island (river km 34) to East Sand Island (river...
Arenig volcanic and sedimentary strata, central New Brunswick and eastern Maine
W. H. Poole, Robert B. Neuman
2002, Atlantic Geology (38) 109-134
Arenig strata in the Napadogan area of the Miramichi Highlands of west-central New Brunswick are similar to those of the Lunksoos anti-clinorial area of eastern Maine. Strata from both areas were deposited in a volcanic back-arc setting upon Cambrian-Tremadoc, deep-water, turbiditic quartzose strata on the northwest-facing Gander margin of Gondwana....
An upwelling model for the Phosphoria sea: A Permian, ocean-margin sea in the northwest United States
D.Z. Piper, P. K. Link
2002, American Association of Petroleum Geologists Bulletin (86) 1217-1235
The Permian Phosphoria Formation, a petroleum source rock and world-class phosphate deposit, was deposited in an epicratonic successor basin on the western margin of North America. We calculate the seawater circulation in the basin during deposition of the lower ore zone in the Meade Peak Member from the accumulation rates...
Seismic structure of the crust and uppermost mantle of North America and adjacent oceanic basins: A synthesis
G.S. Chulick, Walter D. Mooney
2002, Bulletin of the Seismological Society of America (92) 2478-2492
We present a new set of contour maps of the seismic structure of North America and the surrounding ocean basins. These maps include the crustal thickness, whole-crustal average P-wave and S-wave velocity, and seismic velocity of the uppermost mantle, that is, Pn and Sn. We found the following: (1) The average thickness...
Assessing mine drainage pH from the color and spectral reflectance of chemical precipitates
D.J. Williams, J.M. Bigham, C.A. Cravotta III, S.J. Traina, J.E. Anderson, J.G. Lyon
2002, Applied Geochemistry (17) 1273-1286
The pH of mine impacted waters was estimated from the spectral reflectance of resident sediments composed mostly of chemical precipitates. Mine drainage sediments were collected from sites in the Anthracite Region of eastern Pennsylvania, representing acid to near neutral pH. Sediments occurring in acidic waters contained primarily schwertmannite and goethite...
Seismological evidence for a sub-volcanic arc mantle wedge beneath the Denali volcanic gap, Alaska
D.E. McNamara, M.E. Pasyanos
2002, Geophysical Research Letters (29) 61-1-61-4
Arc volcanism in Alaska is strongly correlated with the 100 km depth contour of the western Aluetian Wadati-Benioff zone. Above the eastern portion of the Wadati-Benioff zone however, there is a distinct lack of volcanism (the Denali volcanic gap). We observe high Poisson's ratio values (0.29-0.33) over the entire length...
Magnetostratigraphy, paleomagnetic correlation, and deformation of pleistocene deposits in the south central Puget Lowland, Washington
J.T. Hagstrum, D. B. Booth, K. G. Troost, R.J. Blakely
2002, Journal of Geophysical Research B: Solid Earth (107) EPM 6-1-EPM 6-13
Paleomagnetic results from Pleistocene sedimentary deposits in the central Puget Lowland indicate that the region has experienced widespread deformation within the last 780 kyr. Three oriented samples were collected from unaltered fine-grained sediments mostly at sea level to determine the magnetostratigraphy at 83 sites. Of these, 47 have normal, 18...
Fault structure and mechanics of the Hayward Fault, California from double-difference earthquake locations
Felix Waldhause, William L. Ellsworth
2002, Journal of Geophysical Research B: Solid Earth (107) ESE 3-1-ESE 3-15
The relationship between small-magnitude seismicity and large-scale crustal faulting along the Hayward Fault, California, is investigated using a double-difference (DD) earthquake location algorithm. We used the DD method to determine high-resolution hypocenter locations of the seismicity that occurred between 1967 and 1998. The DD technique incorporates catalog travel time data...
Sensitive high resolution ion microprobe (SHRIMP) detrital zircon geochronology provides new evidence for a hidden neoproterozoic foreland basin to the Grenville Orogen in the eastern Midwest, U.S.A
J.O.S. Santos, L.A. Hartmann, N.J. McNaughton, R. M. Easton, R.G. Rea, P.E. Potter
2002, Canadian Journal of Earth Sciences (39) 1505-1515
A sensitive high resolution ion microprobe (SHRIMP) was used in combination with backscattered electron (BSE) and cathodoluminescence (CL) images to determine the age of detrital zircons from sandstones in the Neoproterozoic Middle Run Formation of the eastern Midwest, United States. Eleven samples from seven drill cores of the upper part...
A strategy for estimating the rates of recent United States land-cover changes
Thomas R. Loveland, Terry L. Sohl, S.V. Stehman, Alisa L. Gallant, K. L. Sayler, D.E. Napton
2002, Photogrammetric Engineering and Remote Sensing (68) 1091-1099
Information on the rates of land-use and land-cover change is important in addressing issues ranging from the health of aquatic resources to climate change. Unfortunately, there is a paucity of information on land-use and land-cover change except at very local levels. We describe a strategy for estimating land-cover change across...
Paleoseismology at high latitudes: Seismic disturbance of upper Quaternary deposits along the Castle Mountain fault near Houston, Alaska
Peter J. Haeussler, Timothy C. Best, Christopher F. Waythomas
2002, Geological Society of America Bulletin (114) 1296-1310
Most paleoseismic studies are at low to moderate latitudes. Here we present results from a high-latitude (61°30′ N) trenching study of the Castle Mountain fault in south-central Alaska. This fault is the only one known in the greater Anchorage, Alaska, area with historical seismicity and a Holocene fault scarp. It...
Stream piracy in the Black Hills: A geomorphology lab exercise
Brent J. Zaprowski, Edward B. Evenson, Jack B. Epstein
2002, Journal of Geoscience Education (50) 380-388
The Black Hills of South Dakota exhibits many fine examples of stream piracy that are very suitable for teaching geomorphology lab exercises. This lab goes beyond standard topographic map interpretation by using geologic maps, well logs, gravel provenance and other types of data to teach students about stream piracy. Using...
Use of regional climate model output for hydrologic simulations
L.E. Hay, M.P. Clark, R.L. Wilby, W.J. Gutowski, G.H. Leavesley, Z. Pan, R.W. Arritt, E.S. Takle
2002, Journal of Hydrometeorology (3) 571-590
Daily precipitation and maximum and minimum temperature time series from a regional climate model (RegCM2) configured using the continental United States as a domain and run on a 52-km (approximately) spatial resolution were used as input to a distributed hydrologic model for one rainfall-dominated basin (Alapaha River at Statenville, Georgia)...
A step increase in streamflow in the conterminous United States
G.J. McCabe, D.M. Wolock
2002, Geophysical Research Letters (29) 38-1-38-4
Annual minimum, median, and maximum daily streamflow for 400 sites in the conterminous United States (U.S.), measured during 1941-1999, were examined to identify the temporal and spatial character of changes in streamflow statistics. Results indicate a noticeable increase in annual minimum and median daily streamflow around 1970, and a less...
San Andreas fault zone, California: M≥5.5 earthquake history
Tousson R. Toppozada, D.M. Branum, M.S. Reichle, C.L. Hallstrom
2002, Bulletin of the Seismological Society of America (92) 2555-2601
The San Andreas fault zone has been a very significant source of major California earthquakes. From 1812 to 1906 it generated four major earthquakes of M ∼7 or larger in two pairs on two major portions of the fault. A pair of major earthquakes occurred on the central to southern region, where...
Timing of large earthquakes since A.D. 800 on the Mission Creek strand of the San Andreas fault zone at Thousand Palms Oasis, near Palm Springs, California
T. E. Fumal, M. J. Rymer, G. G. Seitz
2002, Bulletin of the Seismological Society of America (92) 2841-2860
Paleoseismic investigations across the Mission Creek strand of the San Andreas fault at Thousand Palms Oasis indicate that four and probably five surface-rupturing earthquakes occurred during the past 1200 years. Calendar age estimates for these earthquakes are based on a chronological model that incorporates radiocarbon dates from 18 in situ burn layers...
Concordant paleolatitudes for Neoproterozoic ophiolitic rocks of the Trinity Complex, Klamath Mountains, California
E. A. Mankinen, N. Lindsley-Griffin, J. R. Griffin
2002, Journal of Geophysical Research B: Solid Earth (107) EPM 11-1-EPM 11-18
New paleomagnetic results from the eastern Klamath Mountains of northern California show that Neoproterozoic rocks of the Trinity ophiolitic complex and overlying Middle Devonian volcanic rocks are latitudinally concordant with cratonal North America. Combining paleomagnetic data with regional geologic and faunal evidence suggests that the Trinity Complex and related terranes...