Michael F. Sheridan, D. F. Crowder
1964, Open-File Report 64-145
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Publication Extents
Not all publications have extents, not all extents are completely accurateW. H. Bradley
1964, Professional Paper 496-A
Hilton Bernard Evans
1964, Open-File Report 64-51
No abstract available....
R.W. Stallman
1964, Professional Paper 411-E
Akio Ogata
1964, Professional Paper 411-G
Thor N. V. Karlstrom
1964, Professional Paper 443
The Kenai Lowland is part of the Cook Inlet Lowland physiographic subprovince that borders Cook Inlet, a major marine reentrant along the Pacific Ocean coastline of south-central Alaska. The Cook Inlet Lowland occupies a structural trough underlain by rocks of Tertiary age and mantled by Quaternary deposits of varying thicknesses....
J. S. Gatewood, Alfonso Wilson, H. E. Thomas, L. R. Kister
1964, Professional Paper 372-B
The effects of drought are most pronounced on soil moisture, because soil is the prime recipient of the water from precipitation, and upon streamflow, because it is the residual water that is not accepted by or that flows out from the soil and groundwater reservoirs. Studies by statistical correlation of...
P.B. Smith
1964, Professional Paper 429-B
K. L. Wier
1964, Open-File Report 66-154
No abstract available. ...
Richard Goldsmith
1964, Open-File Report 64-62
Priestley Toulmin
1964, Bulletin 1163-A
Peter W. Lipman, E. J. McKay
1964, Open-File Report 64-104
No abstract available....
F.A. Watkins Jr.
1964, Open-File Report 64-159
Robert Schneider
1964, Water Supply Paper 1608-F
The Cenomanian-Turonian formations constitute a highly permeable dolomite and limestone aquifer in central Israel. The aquifer is on the west limb of an anticlinorium that trends north-northeast. In places it may be as much as 800 meters thick, but in the report area, largely the foothills of the Judean-Ephraim Mountains...
Clarence R. Gilbert, G.G. Commons, G. E. Koberg, F.W. Kennon
1964, Water Supply Paper 1779-F
This report presents the results of an investigation into the effects of floodwaterretarding structures in the 39 square miles of the Honey Creek basin above the stream-gaging station near McKinney, during the period October 1952 to September 1959. The number of such structures in the study area was increased from...
Marvin Arthur Pistrang, Fred Kunkel
1964, Water Supply Paper 1779-Y
No abstract available....
C. H. Wayman, H. G. Page, J.B. Robertson
1964, Open-File Report 64-162
Charles L. McGuinness
1964, Circular 492
No abstract available....
Philip M. Cohen
1964, Water Supply Paper 1754
Most of the ground water of economic importance and nearly all the ground water closely associated with the flow o# the Humboldt River in the. 40-mile reach near Winnemucca, Nev., are in unconsolidated sedimentary deposits. These deposits range in age from Pliocene to Recent and range in character from coarse...
K.B. Young
1964, Open-File Report 64-167
The collection of data on the flow of rivers in Wisconsin started on a continuing basis in 1913. A few streamflow records were started in the late 1800's, one as early as 1888 (Chippewa River at Chippewa Falls). Much of the work has been done under cooperative arrangements between the...
Donald R. Albin
1964, Water Supply Paper 1779-G
Windsor Lester Adkison
1964, Open-File Report 64-1
No abstract available. ...
Grover Cleveland Goddard
1964, Water Supply Paper 1761
Burdge Irelan, H.B. Mendieta
1964, Water Supply Paper 1779-K
The Brazos River basin, which makes up 15 percent of the land area of Texas, extends from the High Plains, where altitudes reach 4,200 feet and the average precipitation ranges from 15 to 20 inches a year, to the Gulf of Mexico where the annual rainfall is 45-^50 inches. Large...
G. D. Robinson, A. A. Wanek, W. H. Hays, M. E. McCallum
1964, Professional Paper 505
No abstract available....