Michael H. Frimpter
1973, Open-File Report 73-77
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Publication Extents
Not all publications have extents, not all extents are completely accurateMichael H. Frimpter
1973, Open-File Report 73-78
J.L. Glenn, R. O. Van Atta
1973, Professional Paper 433-M
Michael H. Frimpter
1973, Open-File Report 73-82
Charles K. Phenicie, John R. Lyons
1973, Resource Publication 123
No abstract available....
John David Hem, C. E. Roberson, Carol J. Lind, W.L. Polxer
1973, Water Supply Paper 1827-E
Solutions containing from 10 -5 to 10 -2 moles per liter of aluminum and dissolved silica in various ratios were aged at pH levels between 4 and 10 at 25?C. A colloidal amorphous product having the composition of halloysite was produced in most solutions. It had a consistent and reversible...
D.H. Richter, D. L. Jones
1973, IMAP 749
H. R. Anderson, William Ogilbee
1973, Water Supply Paper 1757-L
The Sokoto Basin of northwestern Nigeria lies in the sub-Saharan Sudan belt of west Africa in a zone of savannah-type vegetation. Rainfall, averaging about 30 inches annually in much of the basin, occurs chiefly in a wet season which lasts from May to October. A prolonged dry season extending from...
George L. Hoffman, Donald L. Hart Jr.
1973, Open-File Report 73-376
Since 1963 use of ground water for irrigation in the Oklahoma panhandle has increased greatly as illustrated by the rapid increase in the number of irrigation wells (fig. 1). Because of increased use of ground water, the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, in 1966...
R.K. Gabrysch
1973, Open-File Report 73-374
Removal of water, oil, and gas from the subsurface in Harris County has caused declines in fluid pressures which in turn have resulted in subsidence of the land surface. One critical area of subsidence is in the area of Burnett, Scott, and Crystal Bays near Baytown. Much of this area...
J.O. Shearman, R.V. Swisshelm Jr.
1973, Open-File Report 74-1094
Keith Brindley Ketner
1973, Open-File Report 73-143
No abstract available. ...
Kenneth L. Lindskov
1973, Open-File Report 73-157
C.F. Keech, J.E. Moore, P. A. Emery
1973, Open-File Report 73-139
A "Level B" study is being made of the Platte River basin in Nebraska. The basin (approximately 40,800 square miles) extends the full length of the State, a distance of nearly 470 miles. The study is a Federal and State interagency effort to formulate a comprehensive plan for the conservation,...
R.F. Norvitch, T.G. Ross, Alex Brietkrietz
1973, Open-File Report 73-203
The water resources were studied within an area whose natural ground-water flow is largely towards the center of the metropolitan area. This area coincides with the extent of the Hinckley Sandstone aquifer. Thus, the general geohydrology of the area bounded by the extent of the Hinckley Sandstone (about 6,000 square...
Henry Bell
1973, Bulletin 1376
Leland V. Page, Lewis C. Shaw
1973, Open-File Report 73-217
Record-breaking floods on Sept. 13, 1971, occurred in some urbanized basins of southeastern Pennsylvania. This flooding resulted from heavy, intermittent thunderstorms on Sept. 11-13, 1971, which produced 8 to 12 inches of rainfall in the basins of Skippack, Stony, and Chester Creeks. Rain was heaviest during mid-day of the 13th....
William J. Randolph, Charles R. Gamble
1973, Open-File Report 73-228
This report has been prepared by the U.S. Geological Survey at the request of Mr. Henry Derthick, Engineer of Structures of the Tennessee Department of Transportation, under the authority of a cooperative agreement between the two agencies. It supplements information contained in a report with the same title dated September...
R. Theodore Hurr, P. A. Schneider Jr.
1973, Open-File Report 73-127
Donald H. Richter, Henry R. Schmoll
1973, Geologic Quadrangle 1062
G. A. Lutz, D. W. Hubbell, H.H. Stevens Jr.
1973, Open-File Report 73-162
Marlin E. Lowry
1973, Open-File Report 73-161
The lithologic equivalents of the Fox Hills Sandstone, Lance Formation, and the Tullock member of the Fort Union Formation, as mapped on the east side of the Powder River Basin, can be recognized throughout the basin; however, the formations are in hydraulic connection and cannot be treated as separate aquifers....
John S. Zogorski, Peter W. Anderson, Owen O. Williams
1973, Open-File Report 73-369
Empirical computation of reaeration coefficients generally requires knowledge of mean velocity and mean depth of a stream. A practical method for obtaining this knowledge is described herein. The method involves time-of-travel, streamflow, and cross-sectional measurements, the development of discharge-velocity curves, streamflow profiles, and the computation of cross-sectional areas. Values for...
J.B. Robertson
1973, Open-File Report 73-237
No abstract available....
S. M. Hindall, Earl L. Skinner
1973, Hydrologic Atlas 453
The purpose of this report is to describe the physical environment, availability, characteristics, distribution, movement, and quailty of water in the Pecatonica-Sugar River basin. In addition, water use and water problems are summarized to give an understanding of man's management of water within the basin....