Ernest Pete Beroni
1955, Open-File Report 55-14
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Page 1399, results 34951 - 34975
Publication Extents
Not all publications have extents, not all extents are completely accuratePhilip Forsyth Fix
1955, Open-File Report 55-45
Oat Hill quicksilver mine, located in the Mayacmas district of northern California, and credited with having produced more than 160,000 flasks of quicksilver, was sampled cooperatively by the Buray of Mines and Geological Survey during 1944. 28 diamond drill holes totaling 8,120 feet were drilled by the Bureau of Mines...
W.H. Goines
1955, Open-File Report 55-48
As a result of heavy rains during the late afternoon and night of May 27, 1954, record-breaking floods occurred on small streams in Panola and Lafayette Counties. All flooding was in rural areas, and no loss of life was reported. The Agriculture Stabilization Committees at Sardis and at Oxford estimated...
R.J. Hackman
1955, Open-File Report 55-54
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...
W.L. Burnham
1955, Open-File Report 55-21
S. G. Brown
1955, Open-File Report 55-20
Eugene Brown, J.W. Crooks
1955, Open-File Report 55-19
H.C. Barksdale
1955, Open-File Report 55-4
No abstract available....
P.E. LaMoreaux
1955, Open-File Report 55-87
Several recent years of drought have emphasized the importance of Alabama's ground-water supplies, a matter of concern to us all. So far we have been blessed in Alabama with ample ground-water, although a combination of increased use, waste, pollution, and drought has brought about critical local water shortages. These problems...
Water Resources Division, U.S. Geological Survey
1955, Open-File Report 55-129
W. B. Langbein
1955, Open-File Report 55-90
Flood discharge is the consequence of many contributing hydrologic events which may be presumed to occur fortuitously and independently, such that the probability of a given flood is the product of the probability of each independent contributing event. Of the many factors that lead to a flood, the two most...
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...
Lynn Crandall
1955, Open-File Report 55-32
With Palisades reservoir in operation there will be many years when the available water supply on Snake River above Milner will be fully utilized by storage in the then existing reservoirs under their established priority rights. Surplus water spilling to waste in past years is shown by the record of...
Ralph H. Wilpolt, Douglas W. Marden
1955, Open-File Report 55-200
No abstract available. ...
Leon V. Davis
1955, Open-File Report 55-36
Prior to 1937, ground-water work in Oklahoma consisted of broad scale early-day reconnaissance and a few brief investigations of local areas. The reconnaissance is distinguished by C. N. Gould's "Geology and Water Resources of Oklahoma" (Water-Supply Paper 148, 1905), which covers about half of the present State of Oklahoma. Among...
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...
G.W. Whetstone
1955, Open-File Report 55-193
S. W. West
1955, Open-File Report 55-192
Ground-water levels in the Whitney terrace area, after many years of rise owing to downward percolation of water from irrigated land, became nearly stabilized by 1935. Strong seasonal water-level fluctuations of 8 to 10 feet, however, are common in the Boise Valley. In recent years, the Whitney terrace has been...
M.A. Warren
1955, Open-File Report 55-189
Gerald A. Waring
1955, Open-File Report 55-188
Robert C. Vorhis
1955, Open-File Report 55-184
The strictly "legal" literature of ground-water use and control -except for a few essays in certain of the law reviews- is quite limited. A larger and more pointful source of information and analysis is the legal-scientific writings of the geologists, hydrologists, meteorologists, engineers and others. When new statutes are to...
F. A. Swenson
1955, Open-File Report 55-180
Ground-water investigations were made by the Ground Water Branch, U. S. Geological Survey, from 1946 to 1954, inclusive, in several parts of Montana. These studies were made as part of the program of the Department of the Interior for development of the Missouri River Basin. Thus, the areas selected for...
R.W. Sundstrom
1955, Open-File Report 55-178
The future of ground-water supplies in Texas presents a problem that is very important to the economy of Texas and to the well-being of almost every citizen of the state. It is of particular importance to more than 580 municipalities using ground water as the sole source of water supply;...
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...