John B. Lyons, D. Gottfried, W.L. Smith, H.W. Jaffe, C. L. Waring
1955, Trace Elements Investigations 523
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Publication Extents
Not all publications have extents, not all extents are completely accurateH.I. Feinstein
1955, Trace Elements Investigations 555
Lynn Glover
1955, Trace Elements Investigations 563
George Walton Walker, Frank W. Osterwald
1955, Trace Elements Investigations 567
M.C. Rabbitt, D.B. Vitaliano, S.T. Vesselowsky, and others
1955, Bulletin 1033-B
Stephen M. Herrick, Robert L. Wait
1955, Open-File Report 55-65
The purpose of this investigation which is being made in cooperation with the Georgia Department of Mines, Mining and Geology, Chatham County, and the City of Savannah, is to determine whether salt-water encroachment has occurred in the principal limestone aquifer in the Savannah area, and, if so, to delimit the...
Eugene Brown, J.W. Crooks
1955, Open-File Report 55-19
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.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
G.W. Hahn
1955, Open-File Report 55-56
No abstract available. ...
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....
C.H. Hardison, O. M. Hackett
1955, Open-File Report 55-57
The subject of this paper as given on the program is "Water Supplies for Irrigation in the Northeast." Both surface-water and ground-water resources are discussed, although with somewhat differing approaches. First we discuss the use of streamflow data in estimating the surface-water supplies available for irrigation use. Then we treat...
S. G. Brown
1955, Open-File Report 55-20
L.A. Heindl
1955, Open-File Report 55-63
The development of the San Manuel copper prospect has greatly increased traffic along State Highway 77. Considerable interest in commercial possibilities along that road has resulted in a request by the Arizona State Land Department for information about the ground-water conditions between Oracle and Oracle Junction. This request came too...
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...
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...
M.C. Rabbitt, D.B. Vitaliano, S.T. Vesselowsky, and others
1955, Bulletin 1033-C
C. G. Paulsen
1955, Open-File Report 55-136
Water Resources Division, U.S. Geological Survey
1955, Open-File Report 55-129
Mary Beth McFarlan, Eloise T. Jacobsen
1955, Open-File Report 55-72
The Clinchfield Coal Company No. 102 well was drilled in the western part of Buchanan County near the Dickinson County line. The well started in the Pennsylvanian Norton formation and originally stopped in the Big Stone Gap shale. It was later deepened during 1950 to a total depth of 5847...
J.O. Joerns
1955, Open-File Report 55-73
The purpose of this investigation was to study quantity, quality, and possible sources of the low flow and spring inflow of the Double Mountain Fork of the Brazos River between the Lubbock sewage disposal plant, 3 miles southeast of Lubbock, and a County Road crossing about 15 miles downstream and...
P.W. Johnson, J.M. Cahill
1955, Open-File Report 55-75
The contemplated construction of an earth-fill flood-control dam on the Gila River in the vicinity of Gila Bend, Ariz., required a preliminary evaluation of the effects of such a structure upon the water supply of the area. The proposed dam would temporarily impound teh occasional floods that constitute the only...
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...