C.E. Price
1960, Open-File Report 60-115
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Page 646, results 16126 - 16150
Publication Extents
Not all publications have extents, not all extents are completely accurateJohn Augustus Baker
1960, Circular 431
The Geological Survey has received numerous inquiries about the effects of proposed changes in the wetland environment. The nature of the inquiries suggests a general confusion in the public mind as to wetland values and an increasing concern by the public with the need for facts as a basis for...
W. B. Langbein, Kathleen T. Iseri
1960, Water Supply Paper 1541-A
Raymond L. Nace
1960, Circular 415
Encyclopedic data on world geography strikingly illustrate the drastic inequity in the distribution of the world's water supply. About 97 percent of the total volume of water is in the world's oceans. The area of continents and islands not under icecaps, glaciers, lakes, and inland seas is about 57.5 million...
James K. Searcy, Clayton H. Hardison, Walter B. Langbein
1960, Water Supply Paper 1541-B
The double.-mass curve is used to check the consistency of many kinds of hydrologic data by comparing data for a single station with that of a pattern composed of the data from several other stations in the area The double-mass curve can be used to adjust inconsistent precipitation data. The...
H.G. Thomasson Jr., F. H. Olmsted, E. F. LeRoux
1960, Water Supply Paper 1464
The area described is confined largely to the valley-floor and foothill lands of Solano County, which lies directly between Sacramento, the State capital, and San Francisco. The area is considered in two subareas: The Putah area, which extends from Putah Creek southward to the Montezuma Hills and from the foothills...
F.W. Kennon, Harold V. Peterson
1960, Water Supply Paper 1475-B
Tate Dalrymple
1960, Water Supply Paper 1543-A
This report describes the method used by the U.S. Geological Survey to determine the magnitude and frequency of momentary peak discharges at any place on a stream, whether a gaging-station record is available or not. The method is applicable to a region of any size, as a river basin or...
James K. Searcy
1960, Water Supply Paper 1541-C
A gaging-station record is a sample of the rate of flow of a stream at a given site. This sample can be used to estimate the magnitude and distribution of future flows if the record is long enough to be representative of the long-term flow of the stream. The reliability...
Alfred Clebsch Jr.
1960, Open-File Report 60-27
Wilbur Nathaniel Palmquist, Francis Ramey Hall
1960, Hydrologic Atlas 25
No abstract available....
E.P. Weeks
1960, Open-File Report 60-152
Francis Ramey Hall, Wilbur Nathaniel Palmquist Jr.
1960, Hydrologic Atlas 19
No abstract available....
Wilbur Nathaniel Palmquist Jr., Wilbur Francis Ramey Hall
1960, Hydrologic Atlas 22
No abstract available....
Wilbur Nathaniel Palmquist Jr., Francis Ramey Hall
1960, Hydrologic Atlas 17
No abstract available....
Verl Richard Wilmarth, D.L. Healey, A. Clebsch Jr., I.J. Winograd, L. Zietz, H. W. Oliver
1960, Open-File Report 60-156
Francis Ramey Hall, Wilbur Nathaniel Palmquist
1960, Hydrologic Atlas 23
No abstract available....
Wilbur Nathaniel Palmquist Jr., Francis Ramey Hall
1960, Hydrologic Atlas 16
No abstract available....
Wilbur Nathaniel Palmquist Jr., Francis Ramey Hall
1960, Hydrologic Atlas 15
No abstract available....
Francis Ramey Hall, Wilbur Nathaniel Palmquist
1960, Hydrologic Atlas 24
No abstract available....
Wilbur Nathaniel Palmquist Jr., Francis Ramey Hall
1960, Hydrologic Atlas 20
No abstract available....
Water Resources Division, U.S. Geological Survey
1960, Hydrologic Atlas 39
No abstract available....
Francis Ramey Hall, Wilbur Nathaniel Palmquist Jr.
1960, Hydrologic Atlas 18
No abstract available....
M.W. Busby, M. A. Benson
1960, International Association of Scientific Hydrology - Bulletin (5) 32-36
The basin characteristics Σal or L ca are useful in hydrologic studies, but existing methods of determining them are either tedious or somewhat inaccurate. The grid method presented herein lessens the amount of tedious labor and provides an accurate measure of either Σal or L ca . An adaptation of the method could be used to compute the...
A. Johnson
1960, International Association of Scientific Hydrology - Bulletin (5) 54-60
Variation in surface elevations of the Nisqually Glacier has been recorded since 1942 by the annual measurement of three profiles across the glacier, designated as nos. 1, 2, and 3, located 0.5, 1.0, and 1.7 miles respectively from the terminus, at approximate mean elevations of 5,250,6,000, and 6,800 feet. A fourth...