Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-4
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Page 5225, results 130601 - 130625
Publication Extents
Not all publications have extents, not all extents are completely accurateBruce R. Johnson
1978, Open-File Report 78-495
E. B. Ekren, F.M. Byers Jr.
1978, Open-File Report 78-917
William Henry Hays, D. H. McIntyre, S. W. Hobbs
1978, Open-File Report 78-1060
Woodward-Clyde Consultants
1978, Open-File Report 78-69
Tau Rho Alpha, Phyllis A. Swenson
1978, Open-File Report 78-82
Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-690
B.B. Hampton, C.M. Wood
1978, Open-File Report 78-437
Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Dallas, Dallas County, Fort Worth, Houston, and San Antonio....
Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-415
P.L. Soule
1978, Open-File Report 78-260
A.J. Froelich
1978, Open-File Report 78-443
Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-600
George W. Shurr
1978, Open-File Report 78-249
Harold J. Prostka, G. F. Embree
1978, Open-File Report 78-1009
Virginia Carter, C.P. Baker
1978, Open-File Report 78-86
Woodward-Clyde Consultants
1978, Open-File Report 78-991
Bela Csejtey Jr., Andrew Griscom
1978, Open-File Report 78-558-C
E. B. Ekren, F.M. Byers Jr.
1978, Open-File Report 78-918
William Clinton Steele, Nairn Albert
1978, Open-File Report 78-73-K
George L. Snyder, Carl E. Hedge
1978, Professional Paper 1041
Major Precambrian and minor Tertiary intrusive rocks northeast of Steamboat Springs in the Park Range between 40°30' and 40°45' N. lat. are described and compared with related rocks elsewhere in Colorado and Wyoming. The Precambrian intrusives were emplaced in a sequence of high-grade interlayered felsic gneisses, amphibolites, and pelitic schists...
Kevin M. Scott, Rhea P. Williams
1978, Professional Paper 1030
Major-storm and long-term erosion rates in mountain watersheds of the western Transverse Ranges of Ventura County, Calif., are estimated to range from low values that would not require the construction of catchments or channel-stabilization structures to values as high as those recorded anywhere for comparable bedrock erodibilities. A major reason...
Marion L. Maderak, J.D. Gordon, R.N. Mitchell
1978, Open-File Report 78-457
Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, Dallas and Dallas County, Fort Worth, Houston, and San Antonio.The Geological Survey, in cooperation with the Texas Department of Water Resources, began hydrologic studies in the Austin...
D.E. Stuart-Alexander
1978, IMAP 1047
This map is one of a series of geologic maps that will cover the entire Moon at a scale of 1:5,000,000. The geology of the central far side is compiled largely from NASA Lunar Orbiter...
E.M. MacKevett Jr.
1978, IMAP 1032
D.L. Hart, Robert Ellis Davis
1978, Open-File Report 78-766
The Antlers aquifer, which consists of as much as 900 feet of friable sandstone, silt, clay, and shale, crops out in area of 1,860 square miles and underlies about 4,400 square miles in southeastern Oklahoma. Precipitation ranges from 34 to 50 inches per year across the outcrop area which is...