J. G. Weathers (compiler), George Plafker
1998, Open-File Report 98-126
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Publication Extents
Not all publications have extents, not all extents are completely accurateP.R. Carlson, T.R. Bruns, K.R. Evans, J. T. Gann, D.J. Hogg, S. James Taggart, P.N. Hooge
1998, Open-File Report 98-134
E. S. Wissinger, A. R. Levander, J. S. Oldow, Gary S. Fuis, W. J. Lutter
1998, Book chapter, Architecture of the central Brooks Range fold and thrust belt, Arctic Alaska
No abstract available....
John E. Gray, James R. Riehle, editor(s)
1998, Professional Paper 1595
This collection of 12 papers continues the annual series of U.S. Geological Survey (USGS) reports on geologic investigations in Alaska. The annual volume presents results from new or ongoing studies in Alaska that are of interest to scientists in academia, industry, land and resource managers, and the general public. The...
Warren E. Yeend, Peter H. Stauffer, James W. Hendley II
1998, Fact Sheet 058-98
Philip A. Baedecker, Jeffrey N. Grossman, Kim P. Buttleman
1998, Data Series 47
The PLUTO CD-ROM data base contains inorganic geothermal data obtained by the analytical laboratories of the Geologic Division of the U.S. Geological Survey (USGS) for the United States, including Hawaii and Alaska, in support of USGS program activities requiring chemical data. This CD-ROM was produced in accordance with the ISO...
Judy Fierstein, Wes Hildreth, James W. Hendley II, Peter H. Stauffer
1998, Fact Sheet 075-98
Kathleen A. McCarthy, Michael R. Lilly, Joan F. Braddock, Larry D. Hinzman
1998, Open-File Report 98-198
Natural attenuation processes include biological degradation, by which microorganisms break down contaminants into simpler product compounds; adsorption of contaminants to soil particles, which decreases the mass of contaminants dissolved in ground water; and dispersion, which decreases dissolved contaminant concentrations through dilution. The primary objectives of this study are to (1)...
P. B. O’Sullivan, Thomas E. Moore, J.M. Murphy
J. S. Oldow, H.G. Ave Lallemant, editor(s)
1998, Book chapter, Architecture of a fold and thrust belt: Central Brooks Range, Arctic Alaska
The Mt. Doonerak antiform is a northeast-trending, doubly plunging antiform located along the axial part of the central Brooks Range. This antiform is a crustal-scale duplex estimated to have a vertical displacement of ~15 km. The antiform folds the Amawk thrust, which separates relatively less displaced lower plate rocks in...
D.H. Richter, R.B. Symonds, D. S. Rosenkrans, R. G. McGimsey, William C. Evans, R.J. Poreda
1998, Open-File Report 98-128
G. S. Fuis
1998, Tectonophysics (288) 265-292
A comparison of the deep structure along nine recent transects of the west margin of North America shows many important similarities and differences. Common tectonic elements identified in the deep structure along these transects include actively subducting oceanic crust, accreted oceanic/arc (or oceanic-like) lithosphere of Mesozoic through Cenozoic ages. Cenozoic...
Tuula E. Hollmen, J. Christian Franson, Lynn H. Creekmore, Joel A. Schmutz, Ada C. Fowler
1998, Condor (100) 402-404
We surveyed Emperor Geese (Chen canagica) in western Alaska for avian hematozoa. Blood smears were collected from 134 adults and goslings in late July 1996, on their breeding grounds on the Yukon-Kuskokwim Delta. One of 134 (0.7%) Emperor Geese harbored Leucocytozoon simondi, representing a new host record for this parasite. No...
Water Resources Division, U.S. Geological Survey
1998, Fact Sheet 012-98
As United States coal resources continue to be examined for potential development, a critical need exists for a digital database containing locations and status of all Federal coal resources. This Fact Sheet describes the development of such a digital database and presents examples of how the U.S. Geological Survey (USGS)...
Joseph D. Kaplan, Michael W. Meyer, Peter S. Reaman, W. Emmett Braselton, A. Major, Neil Burgess, Anton M. Scheuhammer
1998, Environmental Toxicology and Chemistry (17) 173-183
The common loon (Gavia immer) is a high‐trophic‐level, long‐lived, obligate piscivore at risk from elevated levels of Hg through biomagnification and bioaccumulation. From 1991 to 1996 feather (n = 455) and blood (n = 381) samples from adult loons were collected between June and September in five regions of North America: Alaska,...
A.L. Wright, G.D. Hayward, Steven M. Matsuoka, P.H. Hayward
1998, The Birds of North America
No abstract available...
Warren J. Nokleberg, Nikolai A. Goryachev, Vladimir I. Shpikerman, Thomas K. Bundtzen, Alexander I. Khanchuk, Vladimir V. Ratkin, Leonid M. Parfenov
R. Seltmann, G.A. Gonevchuk, Alexander I. Khanchuk, editor(s)
1998, Book, Anatomy and textures of ore-bearing granitoids of Sikhote Alin (Primorye Region, Russia) and related mineralization: extended abstracts
J. D. Phillips, R. W. Saltus, R. L. Reynolds
1998, Book chapter, Geologic applications of gravity and magnetics: case histories
No abstract available....
J.F. Meyer Jr., L.J. Racic, R. W. Saltus
1998, Book chapter, Geologic applications of gravity and magnetics: case histories
No abstract available....
V.G. Barnes Jr., R. B. Smith
1998, Ursus (10) 1-9
During 1987-94 we used capture-mark-resight (CMR) methodology and rates of observation (bears/hour and bears/100 km2) of unmarked brown bears (Ursus arctos middendorffi) during intensive aerial surveys (IAS) to estimate abundance of brown bears on Kodiak Island and to establish a baseline for monitoring population trends. CMR estimates were obtained on 3 study areas; density ranged...
J. Christian Franson, Margaret R. Petersen, Lynn H. Creekmore, Paul L. Flint, Milton R. Smith
1998, Ecotoxicology (7) 175-181
We collected, 342 blood samples from spectacled eiders (Somateria fischeri) on their breeding grounds in western Alaska from late May through to early August 1993–1995. Lead concentrations of ≥0.50 p.p.m. wet weight were found in the blood of 20% of the adult female eiders, 2% of the adult...
Alisa A. Abookire, Brenda L. Norcross
1998, Journal of Sea Research (39) 113-123
Three transects in Kachemak Bay, Alaska, were sampled in September 1994, May and August 1995, and February, May, and August 1996. Juvenile flathead sole, Hippoglossoides elassodon, and rock sole, Pleuronectes bilineatus, were the most abundant flatfishes, comprising 65-85% of all fiatfishes captured at any period. Collections of fish and sediments...
William D. Ostrand, Kenneth O. Coyle, Gary S. Drew, John M. Maniscalco, David B. Irons
1998, The Condor (100) 286-297
We collected hydroacoustic and bird-observation data simultaneously along transects in three areas in Prince William Sound, Alaska, 21 July-11 August 1995. The probability of the association of fish schools with Marbled Murrelets (Brachyramphus marmoratus) and Tufted Puffins (Fratercula cirrhata) was determined through the use of resource selection functions based on...
M.R. Dobson, D. O'Leary, M. Veart
1998, Geological Society Special Publication (129) 43-66
Sediment delivery to the Gulf of Alaska occurs via four areally extensive deepwater fans, sourced from grounded tidewater glaciers. During periods of climatic cooling, glaciers cross a narrow shelf and discharge sediment down the continental slope. Because the coastal terrain is dominated by fjords and a narrow, high-relief Pacific watershed,...
John M. Pearce, Daniel Esler, Andrei G. Degtyarev
1998, Wildfowl (49) 110-123
In 1994 and 1995 we investigated breeding biology and nest site habitat of Spectacled Eiders on two study areas within the coastal fringe of the Indigirka River Delta, Russia (71°20' N, 150°20' E). Spectacled Eiders were first observed on 6 June in both years and nesting commenced by mid-June. Average...
J.S. Davis, Sarah M. Roeske, Susan M. Karl
1998, Journal of Structural Geology (20) 639-654
Shear zones in the Late Cretaceous Sitka Graywacke of the Chugach accretionary complex in southeast Alaska record constrictional finite strains, with maximum principal s tretches plunging shallowly subparallel to strike of the shear zones. Macrostructural analysis indicates the finite strain formed during one deformation event. Microstructural analysis of the shear...