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Page 2562, results 64026 - 64050

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Numbered nasal discs for waterfowl
James C. Bartonek, C.W. Dane
1964, Journal of Wildlife Management (28) 688-692
Numbered nasal discs were successfully used in studies requiring large numbers of individually marked waterfowl. The procedure for constructing these discs is outlined. Blue-winged teal (Anas discors) with 5/8-inch discs, and canvasback (Aythya valisineria) and redhead (A. americana) with 3/4-inch discs can be individually identified up to 50 and 80...
Selected hydrologic data, upper Sevier River basin, Utah
Carl H. Carpenter, Gerald B. Robinson Jr., Louis Jay Bjorklund
1964, Utah Basic-Data Report 8
This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.Records were collected during 1961-63 by the U.S. Geological Survey in cooperation...
Water in the world
Luna Bergere Leopold
1964, The UNESCO Courier (17) 11-13
The earth, Including Its oceans and atmosphere, ls a giant distillation system whose operation brings about the distribution of fresh water throughout the world, from the frozen wastes of polar regions to the burning equatorial deserts. Stated in the simplest terms, distillation, condensation and liquid flow are the elemental processes...
Quality of surface waters in Utah, October 1962 to September 1963
U.S. Geological Survey
1964, Report
This data release is a compilation that presents water-quality data for the period October 1962 to September 1963 for the sites listed on page 2. These preliminary data are subject to revision before final publication in the annual series of U.S. Geological Survey Water-supply papers entitled Quality of surface waters...
Ground-water data, Sevier Desert, Utah
Reed W. Mower, Richard D. Feltis
1964, Utah Basic-Data Report 9
This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.Records were collected during the period 1935-64 by the U.S. Geological survey...
[Book review] Politics and water resources
Luna Bergere Leopold
1964, Science (144) 402-403
Arizona is a state in which development has proceeded sufficiently rapidly relative to the available water supply that its water problems are as acute as those of nearly any other state in the Union. Owing to the fact that, in the past, the principal use of water was for irrigation,...
Fluvial processes in geomorphology
Luna Bergere Leopold, M. Gordon Wolman, John P. Miller
1964, Book
This excellent text is a pioneering work in the study of landform development under processes associated with running water. Its primary emphasis is on subjects that were the focus of the authors' studies in both field and laboratory. Part I deals with the process of change in the evolving landscape....
Developing a State Water Plan: A basic water resource data program for Utah
Ted Arnow, R.H. Langford, M. T. Wilson
1964, Cooperative Investigations Report 1
Reliable data on Utah's water resources are essential to development of a State Water plan. While the need for such data was outlined in the report entitles "Developing a State Water Plan - Utah's water resources, problems, and needs - A challenge" published by the Utah Water and Power Board...
Origin of precambrian iron formations
H. Lepp, S. S. Goldich
1964, Economic Geology (59) 1025-1060
A statistical study of the chemical composition of the Precambrian iron formations of the Canadian Shield affords a new approach to the origin of these unusual formations. The average total iron content of 2,200 samples from the literature and from unpublished mining company analyses is 26.7 percent Fe. The average Fe content for 16 iron formations in the United States and Canada...
Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data
D. C. Hahl, C.G. Mitchell
1963, Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-I
This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part...
Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah
R. W. Mower
1963, Utah State Engineer Water Circular 10
Ground water occurs in a shallow (unconfined) aquifer and in at least two artesian (confined) aquifers in the unconsolidated alluvial material composing the valley fill near Sugarville, Utah. No wells are known to withdraw water from the unconfined aquifer, and this report is limited to a discussion of the effects...
Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah
R.D. Feltis, G.B. Robinson
1963, Utah State Engineer Water Circular 12
A test-drilling program was conducted by the U.S. Geological Survey in the upper Sevier River drainage basin (fig. 1) in the summer of 1962. The program was part of a ground-water investigation made in cooperation with the Utah State Engineer. The drilling was financed cooperatively through the State Engineer by...
Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah
Robert M. Cordova
1963, Utah Geological and Mineralogical Survey Water-Resources Bulletin 4
The area investigated comprises 33 square miles in the Price River drainage basin ad is in the High Plateaus section of Utah. Precipitation on most of the area ranges from about 20 to 23 inches per year, and the average annual precipitation for the entire area was assumed to be...
Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61
Ralph E. Smith, Joseph S. Gates
1963, Utah Geological and Mineralogical Survey Water-Resources Bulletin 2
The East Shore area is in north-central Utah between the Wasatch Range and Great Salt Lake, and it has been divided into the Bountiful, Weber Delta, and Brigham ground-water districts, from south to north. The area described in this report includes the Bountiful and Weber Delta districts and the southernmost...
Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania
Harold Meisler
1963, Ground Water Report 18
The Lebanon Valley, which is part of the Great Valley in southeastern Pennsylvania, is underlain by carbonate rocks in the southern part and by shale in the northern part. The carbonate rocks consist of alternating beds of limestone and dolomite of Cambrian and Ordovician age. Although the beds generally dip...
Hydrology of Brooklyn Lake near Keystone Heights, Florida
William E. Clark, Rufus H. Musgrove, Clarence G. Menke, Joseph W. Cagle Jr.
1963, Florida Geological Survey Report of Investigations 33
Brooklyn Lake receded about 20 feet during 1954-58 and reached its lowest stage of record (97.2 feet) in February 1958; this was the lowest stage in the memory of longtime residents. This unusually large recession was a result of deficient rainfall during more than a 3-year period, January 1954 to...
Geology and ground-water resources of northwestern King County, Washington
Bruce A. Liesch, Charles E. Price, Kenneth L. Walters
1963, Water Supply Bulletin 20
King County, in the west-central part of the State of Washington, includes about 2,135 square miles. The eastern part of the county lies in the Sierra-Cascade Mountains province and the remainder is in the Puget Trough of the Pacific Border province. The area covered by the present investigation is almost...
Geology and ground water resources of Kidder County, North Dakota
Jon L. Rau, Wallace E. Bakken, James Chmelik, Barrett J. Williams, P.G. Randich, L. R. Petri, D. G. Adolphson, Edward Bradley
1963, Bulletin 36
Kidder County was covered with glacial ice at least three times during the Wisconsin Stage of the Pleistocene, but the entire sequence of drifts has not been observed in one exposure. The drift which covers the area was deposited during three ice advances termed the Long Lake, Burnstad and Streeter...