R.E. Weems, E. M. Lemon Jr.
1985, Open-File Report 85-378
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Publication Extents
Not all publications have extents, not all extents are completely accurateNicholas M. Ratcliffe
1985, Geologic Quadrangle 1573
F. G. Lesure, S. W. Nicholson
1985, Miscellaneous Field Studies Map 1760-A
J. R. Stone, E.H. London
1985, Miscellaneous Field Studies Map 1524
G. H. Billingsley, C.W. Barnes, G. E. Ulrich
1985, IMAP 1644
M. J. Ellis, R.A. Hiergesell
1985, Water-Resources Investigations Report 85-4195
The practicality of using surface geophysical methods for obtaining geohydrologic data in the Nebraska Sand Hills region was studied during the summer of 1984. Seismic refraction and electrical-resistivity equipment were used, because an evaluation of geohydrologic data indicated that results of surveys made with this equipment probably would yield the...
J. M. Knott, S. W. Lipscomb
1985, Open-File Report 85-157
Water Resources Division, U.S. Geological Survey
1985, Open-File Report 85-59
Lawrence J. Poppe, A.H. Eliason, J.J. Fredericks
1985, Circular 963
The Automated Particle Size Analysis System integrates a settling tube and an electroresistance multichannel particle-size analyzer (Coulter Counter) with a Pro-Comp/gg microcomputer and a Hewlett Packard 2100 MX(HP 2100 MX) minicomputer. This system and its associated software digitize the raw sediment grain-size data, combine the coarse- and fine-fraction data into...
S. C. Wolf, Erk Reimnitz, P. W. Barnes
1985, Open-File Report 85-549
F. B. Gay
1985, Water-Resources Investigations Report 84-4315
Streamflow was the major source of water and nutrients (nitrogen and phosphorus) to Lake Cochituate, followed by ground water, and then precipitation during April 1978 through March 1979. Compared to all sources during that period, streams contributed 7,217 million gallons (a little over 82 percent) of water, 63 ,000 pounds...
Stephen Wolf, P. W. Barnes, Erk Reimnitz
1985, Open-File Report 85-358
S.L. Hanson, D. M. Perkins
1985, Open-File Report 85-615
Lynn A. Yehle, Jack K. Odum, David Reneau
1985, Open-File Report 85-582
Norman J. Page, Floyd Gray
1985, Open-File Report 85-149
M. E. Gettings
1985, Open-File Report 85-26
Mario Fernandez
1985, Water-Resources Investigations Report 84-4301
The Little Manatee River, a coastal stream that empties into Tampa Bay, Florida, may be used as a source of freshwater. Reduction of streamflow will result in upstream movement of saltwater in the stream. Data on streamflow, tide stage, and specific conductance describe the salinity distribution of the estuary. Vertical...
Water Resources Division, U.S. Geological Survey
1985, IMAP 1718
John T. Sun, editor(s)
1985, Circular 883
J.R. Erickson, R. K. Waddell
1985, Water-Resources Investigations Report 85-4066
No abstract available....
K.F. Dennehy, P.B. McMahon
1985, Open-File Report 85-476
Two years of selected hydrologic and micrometeorologic data collected at a low-level radioactive waste burial site near Barnwell, South Carolina are available on magnetic tape in card-image format. Hydrologic data include daily measurements of soil-moisture tension, soil-moisture specific conductance, and soil temperature at four monitoring site locations. Micrometeorlogic data include...
R. A. Wobus, R.B. Chase, G. R. Scott, R. B. Taylor
1985, Miscellaneous Field Studies Map 1762
Berge Exploration Inc.
1985, Open-File Report 80-30
Edward J. Helley, Cheryl Jaworowski
1985, Bulletin 1628
Robert C. Greene
1985, Open-File Report 85-1
Major-element analyses of 26 samples from seven map units of metavolcanic rocks from the Ranyah area are compared with analyses in the literature of rocks from known tectonic settings. The evidence suggests that most of the layered rocks of the Ranyah area originated in immature island arcs. The Khaniq formation...