Skip to main content
U.S. flag

An official website of the United States government

Dot gov

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Https

Secure .gov websites use HTTPS
A lock ( ) or https:// means you’ve safely connected to the .gov website. Share sensitive information only on official, secure websites.

Search Results

10999 results.

Alternate formats: RIS file of the first 3000 search results  |  Download all results as CSV | TSV | Excel  |  RSS feed based on this search  |  JSON version of this page of results

Page 287, results 7151 - 7175

Show results on a map

Publication Extents

Not all publications have extents, not all extents are completely accurate
Mid-crustal flow during Tertiary extension in the Ruby Mountains core complex, Nevada
T. MacCready, A.W. Snoke, J.E. Wright, K. A. Howard
1997, Geological Society of America Bulletin (109) 1576-1594
Structural analysis and geochronologic data indicate a nearly orthogonal, late Eocene–Oligocene flow pattern in migmatitic infrastructure immediately beneath the kilometer-thick, extensional, mylonitic shear zone of the Ruby Mountains metamorphic core complex, Nevada. New U-Pb radiometric dating indicates that the development of a northward-trending lineation in the infrastructure is partly coeval...
Mapping the radon potential of the united states: Examples from the Appalachians
L.C.S. Gundersen, R.R. Schumann
Hopke P.K., editor(s)
1997, Conference Paper, Environment International
The geologic radon potential of the United States was recently assessed by the U.S. Geological Survey. Results indicate that approximately 33% of the U.S. population lives within geologic provinces where the average indoor radon levels have the potential to be greater than 4 pCi/L (147 Bq/m3). Rock types most commonly...
Correlation of Upper Cretaceous strata from Lima Peaks area to Madison Range, southwestern Montana and southeastern Idaho, USA
T. S. Dyman, R. G. Tysdal, W. J. Perry Jr., J. D. Obradovich, J. C. Haley, D. J. Nichols
1997, Cretaceous Research (18) 751-766
An40Ar/39Ar age of 85.81 Ma±0.22 my was obtained on sanidine from a volcanic procellanite bed near the top of the 2135+m-thick Upper Cretaceous Frontier Formation in the Lima Peaks area of southwestern Montana. This early Santonian age, combined with previously determined age data including a palynological age of Cenomanian for...
Progressive deformation of the Chugach accretionary complex, Alaska, during a paleogene ridge-trench encounter
Timothy M. Kusky
1997, Journal of Structural Geology (19) 139-157
The Mesozoic accretionary wedge of south-central Alaska is cut by an array of faults including dextral and sinistral strike-slip faults, synthetic and antithetic thrust faults, and synthetic and antithetic normal faults. The three fault sets are characterized by quartz ± calcite ± chlorite ± prehnite slickensides, and are all relatively...
NDVI, C3 and C4 production, and distributions in Great Plains grassland land cover classes
L.L. Tieszen, Bradley C. Reed, Norman B. Bliss, Bruce K. Wylie, Benjamin D. DeJong
1997, Ecological Applications (7) 59-78
The distributions of C3 and C4 grasses were used to interpret the distribution, seasonal performance, and potential production of grasslands in the Great Plains of North America. Thirteen major grassland seasonal land cover classes were studied with data from three distinct sources. Normalized Difference Vegetation Index (NDVI) data derived from...
Field guide to the Mesozoic accretionary complex along Turnagain Arm and Kachemak Bay, south-central Alaska
Dwight Bradley, Timothy M. Kusky, Susan M. Karl, Peter J. Haeussler
1997, Book chapter, 1997 Guide to the geology of the Kenai Peninsula. Alaska
Turnagain Arm, just east of Anchorage, provides a readily accessible, world-class cross section through a Mesozoic accretionary wedge. Nearly continuous exposures along the Seward Highway, the Alaska Railroad, and the shoreline of Turnagain Arm display the two main constituent units of the Chugach terrane: the McHugh Complex and Valdez Group....
Hazard assessment of inorganics, individually and in mixtures, to two endangered fish in the San Juan River, New Mexico
Steven J. Hamilton, Kevin J. Buhl
1997, Environmental Toxicology (12) 195-209
Acute toxicity tests were conducted for 96 h with larval Colorado squawfish (Ptychocheilus lucius) and razorback sucker (Xyrauchen texanus) in a reconstituted water quality simulating the San Juan River near Shiprock, New Mexico, to determine biological effect concentrations. Tests were conducted with arsenate, copper, selenate, selenite, zinc, and five mixtures...
Boron contents and isotopic compositions of hog manure, selected fertilizers, and water in Minnesota
S.C. Komor
1997, Journal of Environmental Quality (26) 1212-1222
Boron-isotope (δ11B) values may be useful as surrogate tracers of contaminants and indicators of water mixing in agricultural settings. This paper characterizes the B contents and isotopic compositions of hog manure and selected fertilizers, and presents δ11B data for ground and surface water from two agricultural areas. Boron concentrations in...
Data-collection methods and quality-assurance/quality-control procedures used in the study of episodic stream acidification and its effect on fish and aquatic invertebrates in four Catskill Mountain streams, New York, 1988-90
Anthony J. Ranalli, Barry P. Baldigo, Debra Horan-Ross, Ronald V. Allen
1997, Open-File Report 93-137
The U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency, conducted a 20-month study during 1988-90 to evaluate the effects of episodic acidification on fish and aquatic invertebrates in pristine headwater streams in the Catskill Mountains of New York. The study was part of the Episodic Response Project,...
Rapid extension in an Eocene volcanic arc: Structure and paleogeography of an intra-arc half graben in central Idaho
S. U. Janecke, B.F. Hammond, L.W. Snee, J. W. Geissman
1997, Geological Society of America Bulletin (109) 253-267
A study of extension, volcanism, and sedimentation in the middle Eocene Panther Creek half graben in central Idaho shows that it formed rapidly during an episode of voluminous volcanism. The east-southeast-tilted Panther Creek half graben developed across the northeast edge of the largest cauldron complex of the Challis volcanic field...
Late Cenozoic history and slip rates of the Fish Lake Valley, Emigrant Peak, and Deep Springs fault zones, Nevada and California
M.C. Reheis, T. L. Sawyer
1997, Geological Society of America Bulletin (109) 280-299
Several well-dated stratigraphic markers permit detailed assessment of the temporal and spatial variation in slip rates along the interconnected faults of the Fish Lake Valley, Emigrant Peak, and Deep Springs fault zones in west-central Nevada and east-central California. Right-lateral motion on the Fish Lake Valley fault zone apparently began ca....
14C ages and activity for the past 50 ka at Volcán Galeras, Colombia
N.G. Banks, V.M.L. Calvache, S.N. Williams
1997, Journal of Volcanology and Geothermal Research (77) 39-55
Volcán Galeras is the southernmost Colombian volcano with well-recorded historic activity. The volcano is part of a large and complex volcanic center upon which 400,000 people live. Historic activity has centered on a small-volume cone inside the youngest of several large amphitheaters that breach the west flank of the volcano,...
The Chesapeake Bay bolide impact: A convulsive event in Atlantic Coastal Plain evolution
C. Wylie Poag
1997, Sedimentary Geology (108) 45-90
Until recently, Cenozoic evolution of the Atlantic Coastal Plain has been viewed as a subcyclical continuum of deposition and erosion. Marine transgressions alternated with regressions on a slowly subsiding passive continental margin, their orderly succession modified mainly by isostatic adjustments, occasional Appalachian tectonism, and paleoclimatic change. This passive scenario was...
Primitive magmas at five Cascade volcanic fields: Melts from hot, heterogeneous sub-arc mantle
C. R. Bacon, P. E. Bruggman, R.L. Christiansen, M.A. Clynne, J.M. Donnelly-Nolan, W. Hildreth
1997, Canadian Mineralogist (35) 397-423
Major and trace element concentrations, including REE by isotope dilution, and Sr, Nd, Pb, and O isotope ratios have been determined for 38 mafic lavas from the Mount Adams, Crater Lake, Mount Shasta, Medicine Lake, and Lassen volcanic fields, in the Cascade arc, northwestern part of the United States. Many...
Rift-wide correlation of 1.1 Ga Midcontinent rift system basalts: Implications for multiple mantle sources during rift development
S. W. Nicholson, S.B. Shirey, K. J. Schulz, J.C. Green
1997, Canadian Journal of Earth Sciences (34) 504-520
Magmatism that accompanied the 1.1 Ga Midcontinent rift system (MRS) is attributed to the upwelling and decompression melting of a mantle plume beneath North America. Five distinctive flood-basalt compositions are recognized in the rift-related basalt succession along the south shore of western Lake Superior, based on stratigraphically correlated major element, trace...
Variation in thermal tolerance and routine metabolism among spring- and stream dwelling freshwater sculpins (Teleostei: Cottidae) of the southeastern United States
S. J. Walsh, D. C. Haney, C. M. Timmerman
1997, Ecology of Freshwater Fish (6) 84-94
Evolutionary theory predicts that some aquatic organisms may adapt by directional selection to limiting physical environmental conditions, yet empirical data are conflicting. We sought to test the assumption that sculpins (family Cottidae) inhabiting thermally stable springs of the southeastern United States differ in temperature tolerance and metabolism from populations inhabiting...
Effect of wave-enhanced bottom friction on storm-driven circulation in Massachusetts Bay
R. P. Signell, J. H. List
1997, Journal of Waterway, Port, Coastal and Ocean Engineering (123) 233-239
Massachusetts Bay is a shallow (35 m average depth) semienclosed embayment, roughly 100 ?? 50 km, which opens into the Gulf of Maine at its eastern boundary. Surface waves associated with winter storm winds from the northeast cause large sediment resuspension events, and wave and circulation fields during these events...
Jonah field, Sublette County, Wyoming: Gas production from overpressured Upper Cretaceous Lance sandstones of the Green River basin
Scott L. Montgomery, J. W. Robinson
1997, American Association of Petroleum Geologists Bulletin (81) 1049-1062
Jonah field, located in the northwestern Green River basin, Wyoming, produces gas from overpressured fluvial channel sandstones of the Upper Cretaceous Lance Formation. Reservoirs exist in isolated and amalgamated channel facies 10-100 ft (3-30 m) thick and 150-4000 ft (45-1210 m) wide, deposited by meandering and braided streams. Compositional and...
Geostatistical analysis of regional hydraulic conductivity variations in the Snake River Plain aquifer, eastern Idaho
J.A. Welhan, M.F. Reed
1997, Geological Society of America Bulletin (109) 855-868
The regional spatial correlation structure of bulk horizontal hydraulic conductivity (Kb) estimated from published transmissivity data from 79 open boreholes in the fractured basalt aquifer of the eastern Snake River Plain was analyzed with geostatistical methods. The two-dimensional spatial correlation structure of ln...
Ophiolitic basement to the Great Valley forearc basin, California, from seismic and gravity data: Implications for crustal growth at the North American continental margin
N. J. Godfrey, B. C. Beaudoin, S.L. Klemperer, A. Levander, J. Luetgert, A. Meltzer, Walter D. Mooney, A. Trehu
1997, Geological Society of America Bulletin (109) 1536-1562
The nature of the Great Valley basement, whether oceanic or continental, has long been a source of controversy. A velocity model (derived from a 200-km-long east-west reflection-refraction profile collected south of the Mendocino triple junction, northern California, in 1993), further constrained by density and magnetic models, reveals an ophiolite underlying...
Effects of climate change on freshwater ecosystems of the south-eastern United States and the Gulf Coast of Mexico
P. J. Mulholland, G.R. Best, C.C. Coutant, G.M. Hornberger, J.L. Meyer, P.J. Robinson, J.R. Stenberg, R.E. Turner, F. Vera-Herrera, R.G. Wetzel
1997, Hydrological Processes (11) 949-970
The south-eastern United States and Gulf Coast of Mexico is physiographically diverse, although dominated by a broad coastal plain. Much of the region has a humid, warm temperate climate with little seasonality in precipitation but strong seasonality in runoff owing to high rates of summer evapotranspiration. The climate of southern...
The Bishop Tuff: New insights from eruptive stratigraphy
C. J. N. Wilson, W. Hildreth
1997, Journal of Geology (105) 407-439
The 0.76 Ma Bishop Tuff, from Long Valley caldera in eastern California, consists of a widespread fall deposit and voluminous partly welded ignimbrite. The fall deposit (F), exposed over an easterly sector below and adjacent to the ignimbrite, is divided into nine units (F1‐F9), with no significant time breaks, except...
Seismic source study of the Racha-Dzhava (Georgia) earthquake from aftershocks and broad-band teleseismic body-wave records: An example of active nappe tectonics
H. Fuenzalida, L. Rivera, H. Haessler, D. Legrand, H. Philip, L. Dorbath, D. McCormack, S. Arefiev, C. Langer, A. Cisternas
1997, Geophysical Journal International (130) 29-46
The Racha-Dzhava earthquake (Ms=7.0) that occurred on 1991 April 29 at 09:12:48.1 GMT in the southern border of the Great Caucasus is the biggest event ever recorded in the region, stronger than the Spitak earthquake (Ms=6.9) of 1988. A field expedition to the epicentral area was organised and a...