E.G. Sable, M. D. Mangus, R. H. Morris, J. T. Dutro
1984, Miscellaneous Field Studies Map 1670
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Publication Extents
Not all publications have extents, not all extents are completely accurateCharles W. Hedel
1984, Miscellaneous Field Studies Map 1429
The maps in this report are designed to show the location, nature, and age of fault traces and lineaments that are interpreted to be the result of late Quaternary movement along the Surprise Valley and associated faults. These characteristics are important to scientists and engineers who study the surface faulting...
W. D. Johnson
1984, Water-Resources Investigations Report 83-4122-E
No abstract available....
Bradford Butman, John A. Moody
1984, Miscellaneous Field Studies Map 1710
Lydonia Canyon is one of several large submarine canyons that indent the eastern U.S. Continental Shelf along the southern flank of Georges Bank (Index map). This bathymetric map of the upper part of Lydonia Canyon (water depths shallower than about 2,00 m) was prepared as part of a study of...
D.L. Hanneman
1984, Miscellaneous Field Studies Map 1695
N.L. Hatch, R. H. Moench
1984, Miscellaneous Field Studies Map 1594-A
Edwin Roedder
1984, Open-File Report 84-696
S. E. Church, A. B. Ford, V. J. Flanigan, R.B. Stotelmeyer
1984, Miscellaneous Field Studies Map 1652-A
R. B. Colton, J.L. Klockenbrink, M.A. Grosz, E.L. Heffern
1984, Miscellaneous Field Studies Map 1723
L.C. Kjelstrom
1984, Open-File Report 84-52
This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain Rasa (Regional Aquifer System Analysis) study that was initiation in October 1979. Purposes of the RASA study were to (1) refine knowledge of the regional ground-water flow system, (2) determine effects of conjunctive use of...
D. A. Lindsey, G. R. Scott, S. J. Soulliere, B. L. De Angelis
1984, Miscellaneous Field Studies Map 1623
D.H. Amos
1984, Miscellaneous Field Studies Map 1674
R. R. Carlson, R.A. Martin, R. H. Wood
1984, Miscellaneous Field Studies Map 1244-B
No abstract available....
James E. Callahan, D. H. McIntyre, E.F. Cooley, T. M. Cookro
1984, Miscellaneous Field Studies Map 1466-D
The Jerry Peak Wilderness Study Area is about 25 mi south of Challis in Custer County, central Idaho (fig. 1). The study area contains 46,150 acres of land administered by the by the Bureau of Land Management and 1 sq mi owned by the State of Idaho, a total of...
R.J. Goldfarb, D. L. Leach, J. A. Domenico, S. M. Smaglik
1984, Miscellaneous Field Studies Map 1651-B
R. P. Fogelman, J.R. Mullen, W.F. Shelton, R.G. Simpson
1984, Water Data Report CA-82-4
Water-resources data for the 1982 water year for California consists of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 4 contains discharge records for 163 gaging stations; stage and contents for 27 lakes...
R. C. Greene
1984, Open-File Report 84-327
Jane Hammarstrom
1984, Open-File Report 84-652
Gary L. Gallino, Thomas C. Pierson
1984, Open-File Report 84-578
At approximately 9 p.m. on December 25, 1980, intense rainfall and extremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 cubic yards at the head of Polallie Creek Canyon on the northeast flank of Mount Hood. The landslide was transformed rapidly into a debris flow, which surged...
S. J. Sutley, K.A. Duttweiler, R.T. Hopkins
1984, Open-File Report 84-412
No abstract available....
A. G. Fountain, M.A. Fulk
1984, Open-File Report 84-441
Water Resources Division, U.S. Geological Survey
1984, IMAP 1588
C. A. Perry
1984, Water-Resources Investigations Report 84-4164
Relationships between flood volume and peak discharge in western Kansas were developed considering basin and climatic characteristics in order to evaluate the availability of surface water in the area. Multiple-regression analyses revealed a relationship between flood volume, peak discharge, channel slope , and storm duration for basins smaller than 1,503...
Larry F. Land
1984, Open-File Report 84-817
The importance of the Edwards aquifer as a freshwater resource and its susceptibility to being contaminated, being over utilized, or both resulted in the development of a proposed 10-year plan to monitor and study its hydrology. The plan proposes adjustments to the current monitoring activities of computing and measuring recharge,...
J.S. Havens
1984, Open-File Report 84-808
The data contained in this report were gathered during the period 1982 to 1984 for use in constructing a digital model of the North Canadian River from Lake Overholser, in the western part of Oklahoma City, to Lake Eufaula, in eastern Oklahoma. Locations of test holes and sampling sites are...