Spark ablation-inductively coupled plasma spectrometry for analysis of geologic materials
D. W. Golightly, A. Montaser, B.L. Smith, A. F. Dorrzapf Jr.
1989, Talanta (36) 299-303
Spark ablation—inductively coupled plasma (SA-ICP) spectrometry is applied to the measurement of hafnium—zirconium ratios in zircons and to the determination of cerium, cobalt, iron, lead, nickel and phosphorus in ferromanganese nodules. Six operating parameters used for the high-voltage spark and argon-ICP combination are established by sequential simplex optimization of both...
Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee
Patrick Tucci, D. W. Hanchar
1989, Water-Resources Investigations Report 88-4197
Nineteen wells were installed at nine sites in the Melton Valley area. The wells are intended to provide information on water levels in both regolith and bedrock, aquifer characteristics, and subsurface lithology. Well depths range from 24 to 86 ft for shallow wells, and from 126 to 301 ft for...
Water quality data for precipitation and storm runoff in Pennypack Creek Basin, Philadelphia, Pennsylvania
D.W. Speight
1989, Open-File Report 86-140
This report presents data on the chemistry of precipitation and storm runoff that were collected during 29 storms from July 1979 through November 1980, in an urban environment in the Pennypack Creek basin, Philadelphia, Pennsylvania. Daily mean and instantaneous stream discharge data were collected at two U.S. Geological Survey gaging...
Assessment of processes affecting low-flow water quality of Cedar Creek, west-central Illinois
Arthur R. Schmidt, W.O. Freeman, R.D. McFarlane
1989, Water-Resources Investigations Report 88-4141
Water quality and the processes that affect dissolved oxygen, nutrient (nitrogen and phosphorus species), and algal concentrations were evaluated for a 23.8-mile reach of Cedar Creek near Galesburg, west-central Illinois, during periods of warm-weather, low-flow conditions. Water quality samples were collected and stream conditions were measured over a diel (24...
Maps, sections, and structure-contour diagrams showing the geology and geochemistry of the Mouat nickel-copper prospect, Stillwater complex, Stillwater County, Montana
M. L. Zientek, W.J. Bawiec, N.J. Page, R.W. Cooper
1989, Miscellaneous Field Studies Map 2038
Map showing the distribution of sum of the ranks for concentrations of lead + zinc + copper + silver and lead + zinc in samples of stream sediment from the Wallace 1 degree by 2 degrees Quadrangle, Montana and Idaho
D. L. Leach, R.J. Goldfarb
1989, Miscellaneous Field Studies Map 1354-D
No abstract available. ...
The vertical distribution of selected trace metals and organic compounds in bottom materials of the proposed lower Columbia River export channel, Oregon, 1984
Gregory J. Fuhrer, Arthur J. Horowitz
1989, Water-Resources Investigations Report 88-4099
A proposal to deepen the lower Columbia River navigation channel in Oregon prompted a study of the vertical distribution of selected trace metals and organic compounds in bottom sediments. These data are needed to evaluate the effects of dredging and disposal operations. Elutriation testing of bottom material indicated chemical concentrations...
Quality of bottom material and elutriates in the lower Willamette River, Portland Harbor, Oregon
Gregory J. Fuhrer
1989, Water-Resources Investigations Report 89-4005
In October 1983 the U.S. Geological Survey, in cooperation with the U.S. Army Corp of Engineers, collected bottom-material and water samples from Portland Harbor, Oregon to determine concentrations of trace metals and organic compounds in elutriate-test filtrate and bottom material. Of the trace metals examined in bottom material, concentrations of...
Water quality in Reedy Fork and Buffalo Creek basins in the Greensboro area, North Carolina, 1986-87
M.S. Davenport
1989, Water-Resources Investigations Report 88-4210
Water and bottom-sediment samples were collected from April 1986 through September 1987 at 19 sites in Guilford County and the City of Greensboro, North Carolina. Sampling locations included 13 stream sites, two lakes that supply the City of Greensboro with drinking water, two City of Greensboro finished drinking-water filtration plants,...
Mineral resources of the Mount Tipton Wilderness Study Area, Mohave County, Arizona
Robert C. Greene, Robert L. Turner, Robert C. Jachens, William A. Lawson, Carl L. Almquist
1989, Bulletin 1737-B
The Mount Tipton Wilderness Study Area (AZ-020-012/ 042) comprises 33,950 acres in Mohave County, Ariz. At the request of the U.S. Bureau of Land Management, this area was evaluated for identified mineral resources (known) and mineral resource potential (undiscovered). This work was carried out by the U.S. Bureau of Mines...
The United States Geological Survey: 1879-1989
Mary C. Rabbitt
1989, Circular 1050
The United States Geological Survey was established on March 3, 1879, just a few hours before the mandatory close of the final session of the 45th Congress, when President Rutherford B. Hayes signed the bill appropriating money for sundry civil expenses of the Federal Government for the fiscal year beginning...
Geologic map of the Valdez A-4, B-3, B-4, C-3, C-4, and D-4 quadrangles, northern Chugach Mountains and southern Copper River basin, Alaska
George Plafker, J. S. Lull, W. J. Nokleberg, G. H. Pessel, W. K. Wallace, G. R. Winkler
1989, Open-File Report 89-569
No abstract available....
Analyses of stream sediment samples from the Orange County copper district, east-central Vermont
B.F. Adrian, J. E. Gray, B. F. Arbogast, A.A. Roemer, P.J. Atelsek
1989, Open-File Report 89-544
Bedrock geology of the Bristol quadrangle, Hartford, Litchfield, and New Haven Counties, Connecticut
Howard E. Simpson
1989, Bulletin 1573
Metamorphosed strata of sedimentary origin underlie the upland surface of western Connecticut, and nonmetamorphosed sedimentary strata underlie the adjacent lowland surface of central Connecticut. The metamorphic rocks consist chiefly of micaceous schists and gneisses, with minor amounts of pegmatite, amphibolite, and metaquartzite. These rocks represent three formations. They are, in...
Copper deficiency in Tule Elk at Point Reyes, California
Peter J.P. Gogan, David A. Jessup, Mark Akeson
1989, Journal of Range Management (42) 233-238
Tule elk (Cervus elaphus nannodes) reintroduced to Point Reyes, Calif., in 1978 exhibited gross signs of copper deficiency by June 1979. Copper levels in liver (x=5.9 ppm) and serum (0.42 ppm) of elk in Point Reyes were below levels in adult tule elk from other locations in California (liver,...
Suggestions for prospecting
Water Resources Division, U.S. Geological Survey
1989, Report
Prospectors have contributed much to the development of this Nation's mineral resources. Since the time of the earliest settlement, the need for iron for tools and guns, lead for bullets, and copper for utensils has prompted a search for sources of these metals. The lure of gold and silver provided...
Effects of land use on the water quality and biota of three streams in the Piedmont province of North Carolina
J. K. Crawford, D. R. Lenat
1989, Water-Resources Investigations Report 89-4007
Three small streams in North Carolina 's northern Piedmont were studied to compare the effects of land use in their watersheds on water quality characteristics and aquatic biota. Devil 's Cradle Creek (agricultural watershed) had more than two times the sediment yield of Smith Creek (forested watershed) (0.34 tons/acre compared...
Statistical and simulation analysis of hydraulic-conductivity data for Bear Creek and Melton Valleys, Oak Ridge Reservation, Tennessee
J. F. Connell, Z. C. Bailey
1989, Water-Resources Investigations Report 89-4062
A total of 338 single-well aquifer tests from Bear Creek and Melton Valley, Tennessee were statistically grouped to estimate hydraulic conductivities for the geologic formations in the valleys. A cross-sectional simulation model linked to a regression model was used to further refine the statistical estimates for each of the formations...
Coprecipitation and redox reactions of manganese oxides with copper and nickel
J.D. Hem, Carol J. Lind, C. E. Roberson
1989, Geochimica et Cosmochimica Acta (53) 2811-2822
Open-system, continuous-titration experiments have been done in which a slow flux of ∼0.02 molar solution of Mn2+ chloride, nitrate, or perchlorate with Cu2+ or Ni2+ in lesser concentrations was introduced into an aerated reactor solution held at constant temperature and at constant pH by a pH-stat...
Late Cretaceous paleomagnetism and clockwise rotation of the Silver Bell Mountains, south central Arizona
J.T. Hagstrum, D.A. Sawyer
1989, Journal of Geophysical Research Solid Earth (94) 17847-17860
Late Cretaceous ash flow volcanism in the Silver Bell Mountains of southern Arizona (32.3°N, 248.5°E) was associated with caldera formation and porphyry copper mineralization. Oriented samples from 34 sites in volcanic, volcaniclastic, and intrusive units related to this episode of igneous activity (73–69 Ma) yield a mean paleomagnetic direction of I =...
Physical and chemical characteristics of a metal-contaminated overbank deposit, west-central South Dakota, USA
D. C. Marron
1989, Earth Surface Processes and Landforms (14) 419-432
The deposit along the Belle Fourche River is typically up to 2 m thick and extends about 90 m away from the channel along the insides of meander bends. The sediments contain above-background levels of copper, iron, manganese, zinc, and particularly arsenic. An influx at high streamflow of uncontaminated sediment...
A high-resolution seismic reflection/refraction study of the Chugach-Peninsular terrane boundary, southern Alaska
T.M. Brocher, M. A. Fisher, E.L. Geist, N.I. Christensen
1989, Journal of Geophysical Research Solid Earth (94) 4441-4455
We present results from a high-resolution seismic refraction analysis of the shallow (approximately 2 km) crustal structure along the 107-km-long Trans-Alaska Crustal Transect Chugach reflection line in southern Alaska and a comparison with laboratory measurements of field samples. The refraction analysis includes the two-dimensional interpretation of several thousand first- and...
Trace metal associations in the water column of South San Francisco Bay, California
J.S. Kuwabara, Cecily C.Y. Chang, J. E. Cloern, T. L. Fries, J.A. Davis, S. N. Luoma
1989, Estuarine, Coastal and Shelf Science (28) 307-325
Spatial distributions of copper (Cu), zinc (Zn) and cadmium (Cd) were followed along a longitudinal gradient of dissolved organic carbon (DOC) in South San Francisco Bay (herein referred to as the South Bay). Dissolved Cu, Zn and Cd concentrations ranged from 24 to...
Paleohydrologic evolution and geochemical dynamics of cumulative supergene metal enrichment at La Escondida, Atacama Desert, northern Chile
Charles N. Alpers, G.H. Brimhall
1989, Economic Geology (84) 229-255
Quantitative limonite mapping within the leached capping of the porphyry copper deposit at La Escondida, Chile, permits reconstruction of the paleohydrologic and chemical evolution of a well-developed supergene ore-forming system. The mineralogy, textures, and relative abundance of supergene limonite minerals (hematite, goethite, and jarosite) are used to reconstruct the former...
Bedrock geology and tectonic evolution of the Wrangellia, Peninsular, and Chugach terranes along the Trans-Alaska Crustal Transect in the Chugach Mountains and southern Copper River Basin, Alaska
George Plafker, W. J. Nokleberg, J. S. Lull
1989, Journal of Geophysical Research Solid Earth (94) 4255-4295
The Trans-Alaskan Crustal Transect in the southern Copper River Basin and Chugach Mountains traverses the margins of the Peninsular and Wrangellia terranes, and the adjacent accretionary oceanic units of the Chugach terrane to the south. The southern Wrangellia terrane margin consists of a polymetamorphosed magmatic arc complex at least in...