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

11003 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 293, results 7301 - 7325

Show results on a map

Publication Extents

Not all publications have extents, not all extents are completely accurate
Temporal changes in the configuration of the water table in the vicinity of the management systems evaluation area site, central Nebraska
John M. Kilpatrick
1996, Water-Resources Investigations Report 94-4173
To improve understanding of the hydrologic characteristics of the shallow aquifer in the vicinity of the Management Systems Evaluation Area site near Shelton, Nebraska, water levels were measured in approximately 130 observation wells in both June and September 1991. Two water-table maps and a water-level-change map were drawn on the...
Hydrogeologic framework of the North Carolina coastal plain
M. D. Winner Jr., R. W. Coble
1996, Professional Paper 1404-I
The hydrogeologic framework of the North Carolina Coastal Plain aquifer system consists of 10 aquifers separated by 9 confining units. From top to bottom, the aquifers are the surficial aquifer, Yorktown aquifer, Pungo River aquifer, Castle Hayne aquifer, Beaufort aquifer, Peedee aquifer, Black Creek aquifer, upper Cape Fear aquifer, lower...
Hazards and climatic impact of subduction‐zone volcanism: A global and historical perspective
Robert I. Tilling
1996, Book chapter, Subduction: Top to Bottom
Subduction-zone volcanoes account for more than 80 percent of the documented eruptions in recorded history, even though volcanism--deep and, hence, unobserved--along the global oceanic ridge systems overwhelmingly dominates in eruptive output. Because subduction-zone eruptions can be highly explosive, they pose some of the greatest natural hazards to society if the...
Floods, runoff, and snowpack in Utah, 1995
D.V. Allen
1996, Fact Sheet 106-96
Utah, like other States in the western United States, has experienced several rapid and extreme changes between wet and dry precipitation cycles during recent years. During the 1995 water year (October 1994 to September 1995), most areas of Utah experienced greater-than-normal precipitation (1961-90), which was reflected in greater-than-average snowpack, moderate...
Hydrology of the Mississippi River valley alluvial aquifer, south-central United States
D. J. Ackerman
1996, Professional Paper 1416-D
Ground-water flow simulation indicates that pumpage from the aquifer since the early 1900's has caused a decrease in ground-water outflow to rivers, an increase in flow from rivers into the aquifer, and an increase in flow to the aquifer through the overlying confining unit. By the mid-1970's, rivers became a...
Chemical evaluation of soil-solution in acid forest soils
G.B. Lawrence, Mark B. David
1996, Soil Science (161) 298-313
Soil-solution chemistry is commonly studied in forests through the use of soil lysimeters.This approach is impractical for regional survey studies, however, because lysimeter installation and operation is expensive and time consuming. To address these problems, a new technique was developed to compare soil-solution chemistry among red spruce stands in New...
Summary of the Snake River plain Regional Aquifer-System Analysis in Idaho and eastern Oregon
G. F. Lindholm
1996, Professional Paper 1408-A
Regional aquifers underlying the 15,600-square-mile Snake River Plain in southern Idaho and eastern Oregon was studied as part of the U.S. Geological Survey's Regional Aquifer-System Analysis program. The largest and most productive aquifers in the Snake River Plain are composed of Quaternary basalt of the Snake River Group, which underlies...
Crustal and upper mantle velocity structure of the Salton Trough, southeast California
T. Parsons, J. McCarthy
1996, Tectonics (15) 456-471
This paper presents data and modelling results from a crustal and upper mantle wide-angle seismic transect across the Salton Trough region in southeast California. The Salton Trough is a unique part of the Basin and Range province where mid-ocean ridge/transform spreading in the Gulf of California has evolved northward into...
Far-travelled Permian chert of the North Fork terrane, Klamath Mountains, California
Edward A. Mankinen, W. P. Irwin, C.D. Blome
1996, Tectonics (15) 314-328
Permian chert in the North Fork terrane and correlative rocks of the Klamath Mountains province has a remanent magnetization that is prefolding and presumably primary. Paleomagnetic results indicate that the chert formed at a paleolatitude of 8.6° ± 2.5° but in which hemisphere remains uncertain. This finding requires that these...
Hydrogeologic framework of the Great Basin region of Nevada, Utah, and adjacent states
R. W. Plume
1996, Professional Paper 1409-B
Regional aquifer systems in the Great Basin consist of carbonate-rock aquifers in the eastern Great Basin and basin-fill aquifers throughout the region. In the carbonate-rock aquifers, barriers to regional flow include Precambrian crystalline basement, upper Precambrian and Lower Cambrian clastic sedimentary rocks, and Jurassic to Tertiary granitic rocks. Basin-fill aquifers...
Biomass patterns in seagrass meadows of the Laguna Madre, Texas
Christopher P. Onuf
1996, Bulletin of Marine Science (58) 404-420
The Laguna Madre of Texas supports the most extensive seagrass meadows in the western Gulf of Mexico, In 1988 seagrasses covered 730 km2 or about three-quarters of the embayment. Halodule wrightii dominated the entire upper laguna, and total biomass was quite uniform near 160 g˙m-2 throughout. Four species shared dominance in...
Large-scale right-slip displacement on the East San Francisco Bay region fault system, California: Implications for location of late Miocene to Pliocene Pacific plate boundary
R. J. McLaughlin, W.V. Sliter, D. H. Sorg, P.C. Russell, A.M. Sarna-Wojcicki
1996, Tectonics (15) 1-18
A belt of northwardly younging Neogene and Quaternary volcanic rocks and hydrothermal vein systems, together with a distinctive Cretaceous terrane of the Franciscan Complex (the Permanente terrane), exhibits about 160 to 170 km of cumulative dextral offset across faults of the East San Francisco Bay Region (ESFBR) fault system. The...
Organic geochemistry applied to environmental assessments of Prince William Sound, Alaska, after the Exxon Valdez oil spill—a review
A.E. Bence, Keith A. Kvenvolden, M.C. Kennicutt II
1996, Organic Geochemistry (24) 7-42
Organic geochemistry played a major role in the environmental assessments conducted following the Exxon Valdez oil spill, which occurred on March 24, 1989, and released about 258,000 bbls (41 million liters) of Alaska North Slope crude oil into Prince William Sound. Geochemical analyses of more than 15,000 sediment, tar, and biological samples...
40Ar/39Ar whole-rock data constraints on Acadian diagenesis and Alleghanian cleavage in the Martinsburg formation, eastern Pennsylvania
R. P. Wintsch, Michael J. Kunk, Jack B. Epstein
1996, American Journal of Science (296) 766-788
A comparison of 40Ar/39Ar age spectra of whole-rock mudstone and slate samples from the Ordovician Martinsburg Formation at Lehigh Gap, Pennsylvania and stratigraphic and thermal constraints support Alleghanian age for regional slaty cleavage and a late Acadian age for diagenesis in these rocks. Age spectra from mud-stones have a sigmodal shape,...
Using landscape ecology to test hypotheses about large-scale abundance patterns in migratory birds
Curtis H. Flather, John R. Sauer
1996, Ecology (77) 28-35
The hypothesis that Neotropical migrant birds may be undergoing widespread declines due to land use activities on the breeding grounds has been examined primarily by synthesizing results from local studies. Growing concern for the cumulative influence of land use activities on ecological systems has heightened the need for large—scale studies...
Geographic variation in migratory behavior of greater white-fronted geese (Anser albifrons)
Craig R. Ely, John Y. Takekawa
1996, The Auk (113) 889-901
We studied the migration and winter distribution of adult Greater White-fronted Geese (Anser albifrons frontalis) radio-marked on the Yukon-Kuskokwim Delta (YKD) and Bristol Bay Lowlands (BBL) of Alaska from 1987 to 1992. The major autumn staging site for geese from both breeding areas was the Klamath Basin on the California/Oregon...
Taxonomic reassessment of the ichnogenus Beaconichnus and additional examples from the Carboniferous of Kansas, U.S.A.
Luis A. Buatois, M. Gabriela Mángano, Christopher G. Maples, William P. Lanier
1996, Ichnos: An International Journal for Plant and Animal Traces (5) 287-302
The ichnogenus Beaconichnus (Gevers 1973), an arthropod trace fossil, includes very different forms that comprise five ichnospecies, namely B. darwi‐nunt (Gevers 1971), B. gouldi (Gevers 1971), B. ahtarcticum(Gevers 1971), B. giganteum Gevers and Twomey 1982, and B. wrrighti Gevers and Twomey 1982. The original diagnosis of Beaconichnus is rather vague and potentially may accommodate virtually every arthropod trackway described from the fossil record. In...
Block and shear-zone architecture of the Minnesota River Valley subprovince: Implications for late Archean accretionary tectonics
D. L. Southwick, V.W. Chandler
1996, Canadian Journal of Earth Sciences (33) 831-847
The Minnesota River Valley subprovince of the Superior Province is an Archean gneiss terrane composed internally of four crustal blocks bounded by three zones of east-northeast-trending linear geophysical anomalies. Two of the block-bounding zones are verified regional-scale shears. The geological nature of the third boundary has not been established. Potential-field...
Complete migration cycle of golden eagles breeding in northern Quebec
Serge Brodeur, R. DeCarie, D.M. Bird, Mark R. Fuller
1996, The Condor (98) 293-299
Radio tracking via satellite was initiated to study the year-round movements of Golden Eagles(Aquila chrysaetosc anadensis) breeding on the east coast of Hudson Bay, Quebec. In June and August 1992, six Golden Eagles(five adults and one juvenile) were marked, three of which completed their year-round movements. The eagles left their breeding area in mid-...
Sediment distribution on a storm-dominated insular shelf, Luquillo, Puerto Rico, U.S.A.
W. C. Schwab, R. W. Rodriguez, W.W. Danforth, M. H. Gowen
1996, Journal of Coastal Research (12) 147-159
A sea-floor mapping investigation designed to assess the sediment distribution, the movement of the nearshore sand supply, and the fate of sediment eroded from the shoreline was conducted using high-resolution sidescan-sonar, seismic reflection, and sediment sampling techniques on the northern insular shelf of Puerto Rico, off the town of Luquillo....
Riparian vegetation and fluvial geomorphic processes
C.R. Hupp, W. R. Osterkamp
1996, Geomorphology (14) 277-295
Riparian vegetation and fluvial-geomorphic processes and landforms are intimately connected parts of the bottomland landscape. Relations among vegetation, processes, and landforms are described here for representative streams of four areas of the United States: high-gradient streams of the humid east, coastal-plain streams. Great Plains streams, and stream channels of the...
Transition from slab to slabless: Results from the 1993 Mendocino triple junction seismic experiment
B. C. Beaudoin, N. J. Godfrey, S.L. Klemperer, C. Lendl, A.M. Trehu, T.J. Henstock, A. Levander, J.E. Holl, A.S. Meltzer, James H. Luetgert, Walter D. Mooney
1996, Geology (24) 195-199
Three seismic refraction-reflection profiles, part of the Mendocino triple junction seismic experiment, allow us to compare and contrast crust and upper mantle of the North American margin before and after it is modified by passage of the Mendocino triple junction. Upper crustal velocity models reveal an asymmetric Great Valley basin...
Record of middle Pleistocene climate change from Buck Lake, Cascade Range, southern Oregon - Evidence from sediment magnetism, trace-element geochemistry, and pollen
J. G. Rosenbaum, R. L. Reynolds, D.P. Adam, J. Drexler, A.M. Sarna-Wojcicki, G.C. Whitney
1996, Geological Society of America Bulletin (108) 1328-1341
Comparison of systematic variations in sediment magnetic properties to changes in pollen assemblages in middle Pleistocene lake sediments from Buck Lake indicates that the magnetic properties are sensitive to changes in climate. Buck Lake is located in southern Oregon just east of the...
Late Stage 5 Glacio-isostatic Sea in the St. Lawrence Valley, Canada and United States
S. Occhietti, S. Balescu, M. Lamothe, M. Clet, T. Cronin, P. Ferland, P. Pichet
1996, Quaternary Research (45) 128-137
Although post-glacial marine sediments of late Wisconsinan and early Holocene age are common in eastern Canada and the northeastern United States, remnants of older Pleistocene marine sediments are scarce. A fossiliferous marine clay that predates the classical Wisconsinan was recently discovered in the St. Lawrence Valley. A dominantly estuarine environment...