R. W. Davis
1965, Hydrologic Atlas 157
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Publication Extents
Not all publications have extents, not all extents are completely accurateR. W. Davis
1965, Hydrologic Atlas 164
Durward H. Boggess, Christian F. Davis, O. J. Coskery
1965, Hydrologic Atlas 141
Durward H. Boggess, Christian F. Davis, O. J. Coskery
1965, Hydrologic Atlas 135
V. Jeff May, Howard E. Allen
1965, Hydrologic Atlas 203
No abstract available....
Gerald L. Thompson
1965, Water Supply Paper 1809-K
Melt-water channel deposits are among the most important aquifers in southwestern Minnesota, but permeable zones within the deposits are difficult to locate. Interpretation of the depositional history of proglacial channel deposits from aerial photographs and test-hole samples indicates the position of the permeable zones. Generally, the coarse-grained deposits are in...
Paul R. Speer, Charles R. Gamble
1965, Water Supply Paper 1675
This report presents a means of determining the probable magnitude and frequency of floods of any recurrence interval from 1.1 to 50 years at most points on streams in the Ohio River basin except Cumberland and Tennessee River basins.Curves are defined that show the relation between the drainage area and...
D. H. Hart, R. C. Newcomb
1965, Water Supply Paper 1697
The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly,...
R.V. Cushman, R. A. Krieger, John A. McCabe
1965, Water Supply Paper 1475-Q
The increase in the number of visitors during the past several years at Mammoth Cave National Park has rendered the present water supply inadequate. Emergency measures were necessary during August 1962 to supplement the available supply. The Green River is the largest potential source of water supply for Mammoth Cave....
J. P. Akers
1965, Water Supply Paper 1771
The central part of Apache County, Ariz., includes an area of about 3,300 square miles between the Navajo Indian Reservation to the north and U.S. Highway 60 to the south. Sedimentary rocks in the area range from Pennsylvanian to Quaternary in age and from 2,000 to more than 6,000 feet...
F. H. Pauszek, Frederick H. Ruggles
1965, Water Supply Paper 1809-N
Denzel R. Cline
1965, Water Supply Paper 1779-U
The purpose of the ground-water investigation of Dane County, Wis., was to determine the occurrence, movement, quantity, quality, and availability of ground water in the unconsolidated deposits and the underlying bedrock. The relationships between ground water and surface water were studied in general in Dane County and in detail in...
Paul T. Voegeli
1965, Water Supply Paper 1809-G
No abstract available....
Gerald K. Moore
1965, Water Supply Paper 1809-F
The area of western Tennessee underlain by the Claiborne Group is about 7,200 square miles and lies on the east flank of the syncline that forms the Mississippi embayment. It includes the Mississippi Alluvial Plain and part of a dissected upland plateau. The Claiborne Group dips to the northwest at...
Douglas C. Alverson
1965, Water Supply Paper 1576-F
The Fort Belknap Indian Reservation includes an area of 970 square miles in north-central Montana. At its north edge is the Milk River valley, which is underlain by Recent alluvium of the Milk River, glacial deposits, and alluvial deposits of the preglacial Missouri River, which carved and occupied this valley...
Philip M. Cohen
1965, Water Supply Paper 1795
This report, resulting from studies made by the U.S. Geological Survey as part of the interagency Humboldt River Research Project, describes the qualitative and quantitative relations among the components of the hydrologic system in the Winnemucca Reach of the Humboldt River valley. The area studied includes the segment of the...
Natalie D. White, W. F. Hardt
1965, Water Supply Paper 1809-R
Charles Lee Roy Holt
1965, Water Supply Paper 1796
Portage County has abundant resources of generally good quality water and, although water problems exist locally, depletion or general scarcity of water is not likely in the foreseeable future. The county receives annually about 31 inches of precipitation, of which about 21 inches is lost as evaportranspiration. The average annual water...
William Kelly Summers
1965, Water Supply Paper 1809-B
Abundant ground water for irrigation is available in the outwash deposits in western Waushara County, and many more large-capacity wells can be developed in these deposits without seriously lowering the water level. Pumping for irrigation temporarily lowers water levels in the vicinity of the wells but has not lowered regional...
R.J. Pickering, P.H. Carrigan, F.L. Parker
1965, Circular 497
The Clinch River Study is a multiagency effort to evaluate the physical, chemical, and biological effects of the release to de Clinch River of low-level radioactive wastes from the Oak Ridge National Laboratory. The major radionuclides released are ruthenium-106, cesium-137, cobalt-60, and strontium-90. Hydrologic and biologic studies have indicated that...
Robert C. Prill, A.I. Johnson, Donald Arthur Morris
1965, Water Supply Paper 1662-B
The increasing use of ground water from many major aquifers in the United States has required a more thorough understanding of gravity drainage, or specific yield. This report describes one phase of specific yield research by the U.S. Geological Survey's Hydrologic Laboratory in cooperation with the California Department of Water...
Richard A. Young, Carl H. Carpenter
1965, Water Supply Paper 1787
The central Sevier Valley, in the central part of Utah, extends from the town of Kingston to the Yuba Dam and from the Tushar and Valley Mountains and the Pavant Range to the Sevier, Fishlake, Wasatch, and Gunnison Plateaus. A geologic and hydrologic investigation of the valley was made to...
Blair F. Jones
1965, Professional Paper 502-A
Dale J. Nyman
1965, Water Supply Paper 1819-B
The Lichterman well field is scheduled to go into operation early in 1965 to supplement the municipal water-supply system for the city of Memphis, Tenn. Although the initial rate of withdrawal from the well field will be about 8 mgd (million gallons per day), the ultimate design capacity of the...
G. E. Welder, Edwin P. Weeks
1965, Water Supply Paper 1791
The Glendo area of Platte and Carbon Counties, Wyo., about 250 square miles in extent, is in the Great Plains physiographic province. It is bordered on the west by the Laramie Range and on the east by the Hartville uplift. The North Platte River and Horseshoe and Middle Bear Creeks...