J.N. Platt
1955, IMAP 16
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Publication Extents
Not all publications have extents, not all extents are completely accurateW. H. Condon
1955, IMAP 104
Mortimer Hay Staatz, Frank W. Osterwald
1955, Trace Elements Investigations 252
Howard Hamilton Waldron, Leonard Meade Gard
1955, Geologic Quadrangle 56
No abstract available....
Roger Milton Waller
1955, Open-File Report 55-186
In response to a request from the Sanitation and Engineering Section of the Alaska Department of Health, a reconnaissance of the possibility of obtaining ground-water supplies for the five villages in the lower Kuskokwim-Yukon River area was made by the Geological Survey early in June 1955. The five Eskimo villages--Kwethluk,...
Paul P. Orkild
1955, IMAP 111
C. H. Marshall
1955, IMAP 88
E.M. Shoemaker
1955, Miscellaneous Field Studies Map 28
No abstract available....
C. H. Marshall
1955, IMAP 58
J. Hiram Smith
1955, Geologic Quadrangle 62
No abstract available....
Robert Wayne Schnabel (compiler)
1955, Mineral Investigations Resource Map 2
H. C. Riggs
1955, Open-File Report 55-151
Recorded annual flood stages and discharges at 144 gaging stations are listed. Also included are maximum known flood stages and discharges, both at gaging stations and at miscellaneous sites. Using the annual flood discharge at gaging stations a regional analysis of flood magnitudes and frequencies in the state was made....
R.V. Cushman
1955, Open-File Report 55-35
Connecticut has a supply of ground water, most of it of good quality, which is largely undeveloped, and much of which would lend itself to industrial and other uses. Ground water is available in small quantities in nearly all parts of the State, and in moderate to large quantities in...
C. G. Paulsen
1955, Open-File Report 55-135
Winchell Smith, W. L. Heckler
1955, Open-File Report 55-170
R. T. Sniegocki
1955, Open-File Report 55-171
William O. George, Frank A. Welder
1955, Open-File Report 55-47
In response to a request by Colonel Harry O. Fisher, District Engineer of the Fort Worth District of the Corps of Engineers, United States Army (letter of Dec. 13, 1954), a reconnaissance investigation was made of the geology of the Canyon (F-1) reservoir site on the Guadalupe River in Comal...
Harold G. Sisco
1955, Open-File Report 55-165
This report contains records of observation wells and water-level fluctuations for the calendar year 1954 in the Aberdeen-Springfield area, Bingham and Power Counties, Idaho. Systematic observations in the Aberdeen-Springfield area were begun by the Geological Survey in 1952. Each year a progress report is issued and this report is number 3...
C. G. Paulsen
1955, Open-File Report 55-136
Allen Sinnott
1955, Open-File Report 55-164
This memorandum has been prepared in response to a recent inquiry from the city officials of Tappahannock, Essex County, Va., regarding the availability of ground water in the Tappahannock area. The memorandum was prepared as part of the ground-water studies of the Geological Survey in cooperation with the Virginia Division...
R. C. Scott
1955, Open-File Report 55-162
Ground-water possibilities in parts of Bear Lake and Caribou counties, Idaho, were studied briefly, with special reference to the vicinities of Dingle and Montpelier and to the availability of ground water for expected industrial developments. The work was part of the ground-water investigations by the Geological Survey in cooperation with...
Donald Robert Coates, R.L. Cushman, James Lawrence Hatchett
1955, Water Supply Paper 1354
The Douglas basin is part of a large northwest-trending intermontane valley, known as the Sulphur Spring Valley, which lies in southeastern Arizona, and extends into northeastern Sonora, Mexico. Maturely dissected mountains rise abruptly from long alluvial slopes and culminate in peaks 3,000 to 4,000 feet above the valley floor, Bedrock...
John Donald Ryan
1955, Open-File Report 55-155
No abstract available. ...
H. Cecil Spicer, Richard A. McCullough, Frederick K. Mack
1955, Open-File Report 55-174
A search for aquifers in an area immediately north of the Chesapeake and Delaware Canal in New Castle, Del., has been made by an electrical resistivity study. The search located 32 sites that may be underlain by sand and gravel. The thicker deposits are significant with respect to the occurrence...
Thad G. McLaughlin
1955, Open-File Report 55-104
Although the subject of this lecture is supposed to be concerned primarily with the hydraulics of wells, Professor Weers has asked that I also discuss the effects tat geological formations have on the quantity and quality of water available to wells. I will discuss the geology of Colorado in relation...