Water Resources Division, U.S. Geological Survey
1984, Open-File Report 84-313
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1984, Open-File Report 84-34
W.P. Hasbrouck
1984, Open-File Report 84-334
W.P. Hasbrouck
1984, Open-File Report 84-175
Water Resources Division, U.S. Geological Survey
1984, Open-File Report 84-531
Water Resources Division, U.S. Geological Survey
1984, Open-File Report 84-42
Jack Burton Epstein
1984, Professional Paper 1337
Water Resources Division, U.S. Geological Survey
1984, Open-File Report 84-315
Carol A. Finn, W.M. Phillips, D.L. Williams
1984, Open-File Report 84-416
No abstract available....
L.H. Geiger
1984, Open-File Report 84-442
Using U.S. Geological Survey computer programs L149-L153, this report shows how to process water-use data for the functional water-use categories: public supply, rural supply, industrial self-supplied, irrigation, and thermo-electric power generation. The programs are used to selectively retrieve entries and list them in a format suitable for publication. Instructions are...
Robert M. Kosanke
1984, Professional Paper 1318
The usefulness of Pennsylvanian palynomorphs, spores, and pollen grains, as an aid in coal-correlation investigations in the Appalachians, has been known for many years. However, much of this and subsequent information was scattered in the literature or was not from the proposed stratotype area of West Virginia. Investigation of coals...
Water Resources Division, U.S. Geological Survey
1984, IMAP 1499
Keith E. Bargar, Melvin H. Beeson
1984, Professional Paper 1054-B
B. D. Leavy
1984, IMAP 1313-G
No abstract available....
P. W. Lipman, Alan Swenson
1984, IMAP 1323
A.P. LeHuray
1984, Open-File Report 84-112
J.B. Lescinsky, M.B. Coll, R.W. Siwicki
1984, Water Data Report PA-83-3
No abstract available. ...
J.B. Graf
1984, Open-File Report 84-468
Twenty-seven measurements of traveltime and longitudinal dispersion in 10 Illinois streams provide data needed for estimating traveltime of peak concentration of a conservative solute, traveltime of the leading edge of a solute cloud, peak concentration resulting from a given quantity of solute, and passage time of solute past a given...
J.J. Daniels, J. H. Scott
1984, Open-File Report 83-235
The following geophysical well log measurements were made in eleven drill holes above the Colorado School of Mines Experimental Mine at Idaho Springs, Colorado: (1) acoustic velocity (2) resistivity, (3) caliper, (4) gamma-gamma density, (5) neutron-thermal neutron, (6) gamma ray, (7) induced polarization (IP), (8) self potential (SP), and magnetic...
R.F. Madole
1984, Open-File Report 84-223
No abstract available....
J.K. Thompson, F.H. Nichols
1984, Open-File Report 84-759
D. L. Leach, J. A. Domenico
1984, Open-File Report 84-700
No abstract available....
D. A. Ponce, S.B. Kohrn, R. W. Saltus, J.B. Spielman, B. A. Chuchel
1984, Open-File Report 84-387
R.D. Krushensky, A.F. Curet
1984, IMAP 1556
D.C. Thorstenson
1984, Open-File Report 84-72
The definition of a formal thermodynamic activity of electrons in redox reactions appears in the literature of the 1920's. The concept of pe as -log (electron activity) was introduced by Jorgensen in 1945 and popularized in the geochemical literature by Sillen, who considered pe and pH as master variables in...