R.V. Cushman
1967, Open-File Report 67-72
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Page 622, results 15526 - 15550
Publication Extents
Not all publications have extents, not all extents are completely accurateA. T. Alter
1967, Hydrologic Atlas 248
No abstract available....
J. R. Ege, R. D. Carroll, F.A. Welder
1967, Open-File Report 67-87
Approximately 1,400 feet of continuous core was taken .between 800-2,214 feet in depth from USBM/AEC Colorado core hole No. 2. The drill, site is located in the Piceance Creek basin, Rio Blanco County, Colorado. From ground surface the drill hole penetrated 1,120 feet of the Evacuation Creek Member and 1,094...
D. C. Hahl, A.H. Handy
1967, Open-File Report 67-103
No abstract available....
F.D. Trauger
1967, Open-File Report 67-220
Water Resources Division, U.S. Geological Survey
1967, Open-File Report 67-256
R. L. Wait, D. O. Gregg
1967, Open-File Report 67-267
Merlin Wheeler
1967, Open-File Report 67-276
D.L. Hart Jr.
1967, Open-File Report 67-285
The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies;...
Perry Rowley Wood, D.L. Hart
1967, Hydrologic Atlas 250
Granville G. Wyrick
1967, Hydrologic Atlas 264
R.W. Maclay, Thomas C. Winter, G.M. Pike
1967, Hydrologic Atlas 237
The Two Rivers watershed includes two physiographic areas a lake plain and a till plain – within its 1,232 square miles. It lies in parts of Kittson and Roseau counties and includes the drainage basins of the Two Rivers and Joe River. The flat lake plain which extends 15 to 20...
Arthur W. Gosling
1967, Hydrologic Atlas 268
No abstract available....
James W. Crooks, Deric O’Bryan
1967, Hydrologic Atlas 244
George M. Farlekas
1967, Hydrologic Atlas 263
George M. Farlekas
1967, Hydrologic Atlas 246
No abstract available....
William M. McMaster
1967, Water Supply Paper 1839-N
Richard L. Phipps
1967, Professional Paper 485-C
Edward Riley Cox
1967, Water Supply Paper 1828
The hydrology of the Pecos River valley between Lake McMillan and Carlsbad Springs, Eddy County, N. Mex., is influenced by facies changes in rocks of Permian age. Water stored for irrigation leaks from Lake McMillan into evaporite rocks, principally gypsum, of the Seven Rivers Formation and from Lake Avalon into...
Wilbur Tennant Stuart, William J. Schneider, James W. Crooks
1967, Water Supply Paper 1829
Local concentrations of population in the Swatara Creek basin of Pennsylvania find it necessary to store, transport, and treat water because local supplies are either deficient or have been contaminated by disposal of wastes in upstream areas. Water in the basin is available for the deficient areas and for dilution...
Raymond L. Nace
1967, Circular 536
Water supplies are not running out, but time is getting short to stem waste of water and destructive exploitation of the environment before harm is done that may be irreparable. Most of the world's water is oceanic brine. Of the waters on the land, most is frozen in Antarctica and...
A.I. Johnson
1967, Water Supply Paper 1662-D
Specific yield is defined as the ratio of (1) the volume of water that a saturated rock or soil will yield by gravity to (2) the total volume of the rock or soft. Specific yield is usually expressed as a percentage. The value is not definitive, because the quantity of...
F.T. Hidaka, Arthur Angus Garrett
1967, Water Supply Paper 1839-J
Hydrologic data collected in the Cedar and Snoqualmie River basins on the west slope of the Cascade Range have been analyzed to determine the amount of water lost by seepage from Chester Morse Lake and Masonry Pool and the. consequent gain by seepage to the Cedar and South Fork Snoqualmie...
John Isbister
1967, Water Supply Paper 1825
No abstract available....
Charles Franklin Keech, V. H. Dreeszen, Philip A. Emery
1967, Water Supply Paper 1839-F
York County, an area of 575 square miles, is situated on an upland plain in southeast Nebraska. Although tributaries of the Big Blue River have eroded valleys into this plain, much of the original surface is still intact and is characterized by broad shallow undrained depressions. The economy is based...