Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania
A. T. Alter
1966, Open-File Report 66-2
Information on flood conditions plays an important part in the development and use of river valleys. This report presents maps, profiles, and flood-frequency relations developed from past flood experience on the Schuylkill River from Conshohocken to Philadelphia, Pa. The maps and profiles are used to define the areal extent and...
Effects of agricultural conservation practices on the hydrology of Corey Creek basin, Pennsylvania, 1954-60
Benjamin L. Jones
1966, Water Supply Paper 1532-C
Analyses of data collected from two small basins in northern Pennsylvania during the period May 1954 to September 1960 indicated that changes in land use and land treatment have affected suspended- sediment discharge from the basins. Extensive land use and land-treatment changes have taken place in the 12.2-square-mile Corey Creek...
Regional trends in water-well drilling in the United States
Gerald Meyer, Granville G. Wyrick
1966, Circular 533
Between the towns of Macon and Taylorville in central Illinois lies a ridge that is part of a system of ridges and knolls largely composed of sand and gravel. This ridge contains an important aquifer. An extensive electrical earth resistivity survey was conducted over the ridged-drift aquifer. Inversion of the...
Hydrologic inventory of the Lompoc subarea, Santa Ynez River basin, Santa Barbara County, California, 1957-62
R. E. Evenson
1966, Open-File Report 66-42
Hydrologic data collected during the climatically near-average 6-year period of inventory 1957-62 provide the basis for making estimates of supply to and demand from the Lompoc subarea of the Santa Ynez River basin and changes in the quantity of water stored in the deposits of the basin. The hydrologic inventory...
A preliminary evaluation of airborne and spaceborne remote sensing data for hydrologic uses
C.J. Robinove
1966, Open-File Report 67-189
Floods on small streams in Texas
Frederick H. Ruggles Jr.
1966, Open-File Report 66-119
The first streamflow station in Texas was established on the Rio Grande at El Paso on May 10, 1889. Sip,ce that time the systematic collection of streamflow data. has expanded. In 1915 the Texas Board of Water Engineers (now the Texas Water Development Board) entered into a cooperative agreement with...
Salt-water encroachment in southern Nassau and southeastern Queens Counties, Long Island, New York
N.J. Lusczynski, Wolfgang V. Swarzenski
1966, Water Supply Paper 1613-F
Test drilling, extraction of water from cores, electric logging, water sampling, and water-level measurements from 1958 to 1961 provided a suitable basis for a substantial refinement in the definition of the positions, chloride concentrations, and rates of movement of salty water in the intermediate and deep deposits of southern Nassau...
Little Sioux River Basin floods
Harlan H. Schwob
1966, Open-File Report 67-196
Highway engineers and many others use flood stages and discharges in the design of bridges and other structures or operations on the flood plain of a stream. These data are provided in the form of gaging-station and other flood records and as flood profiles. Flood-frequency data are used to compute...
The interior of the Earth, an elementary description
Eugene C. Robertson
1966, Circular 532
Evidence on the structure and composition of the earth's interior comes from (1) observations of surface rocks, (2) geophysical data from earthquakes, flow of heat from the interior, the magnetic field, and gravity, (3) laboratory experiments on surface rocks and minerals, and (4) comparison of the earth with other planets,...
Hydrochemical facies and ground-water flow patterns in northern part of Atlantic Coastal Plain
William Back
1966, Professional Paper 498-A
The part of the Atlantic Coastal Plain that extends from New Jersey through Virginia was selected as a suitable field model in which to study the relationships between geology, hydrology, and chemical character of ground water. The ground-water flow pattern is the principal hydrologic control on the chemical character of...
Ultraviolet investigations for lunar missions
William R. Hemphill, William A. Fischer, J.E. Dornbach
Francis Narin, editor(s)
1966, Advances in Astronautical Sciences (20) 397-415
Preliminary field tests of an active ultraviolet imaging system have shown that it is possible to produce linages of the terrain from distances as great as 75 feet by means of reflected ultraviolet light at wavelengths longer than 3300 A. Minerals that luminesce when exposed to ultraviolet energy have been...
Floods of June 24-25, 1966 in southwest-central North Dakota
Orlo A. Crosby
1966, Report
A severe thunderstorm accompanied by much hail swept through southwest-central North Dakota on the afternoon of June 24. Rainfall of up to 13 inches caused floods higher than any previously known in the area. The isohyetal map (fig. 1) indicates the extent and magnitude of the storm. This map was...
Selected flow characteristics of streams in the Willamette River Basin, Oregon
C. H. Swift III
1966, Report
Flow-duration, annual low-flow, and annual high-flow tables through September 30, 1963, are given in this report for 110 stream-gaging stations in the Willamette and Sandy River basins. These tables summarize the basic data needed to define the streamflow characteristics at the gaging stations. The content of each of the three...
Phase relations involving sphalerite in the Fe-Zn-S system
P. B. Barton Jr., Priestley Toulmin
1966, Economic Geology (61) 815-849
The equilibrium diagram for the Fe-Zn-S System has been worked out in détail from 580° to 850° C. Previous work on this System is proven to be seriously in error and températures heretofore estimated from the "sphalerite geothermometer" are without a sound quantitative foundation. Sphalerite solid solutions lie essentially along the FeS-ZnS join. Neither pyrite nor pyrrhotite takes up appréciable amounts of...
Pumping test methods for determining aquifer characteristics
S.M. Lang
1966, ASTM Special Technical Publication 35-55
Data describing the shape and manner in which the cone of depression forms about a well discharging at a constant rate are used with various formulas to determine the hydraulic characteristics of aquifer materials. The solutions to these formulas generally are graphical and may be used to detect the presence of hydraulic or geologic...
Digital computer methods for water‐quality data
C.O. Morgan, R.J. Dingman, J.M. McNellis
1966, Groundwater (4) 35-42
The digital computer is used on a routine basis in the ground-water program in Kansas for tasks ranging from the listing of water-quality data in tabular and publishable form to statistically and graphically analyzing a mass of data.In the past year a number of computer programs in FORTRAN IV have...
Cohenite in meteorites: A proposed origin
R. Brett
1966, Science (153) 60-62
Cohenite [(Fe, Ni)3C] is found almost exclusively in meteorites containing from 6 to 8 percent nickel (by weight). On the basis of iron-nickel-carbon phase diagrams at 1 atmosphere and of kinetic data, the occurrence of cohenite within this narrow composition range as a low-pressure metastable phase and the nonoccurrence of...
Water resources data for Alaska
Water Resources Division, U.S. Geological Survey
1966, Report
No abstract available....
The design and use of hydrogeologic maps
J.C. Warman, D.R. Wiesnet
1966, Groundwater (4) 25-26
A map should treat the critical problems in a way understandable to the intended reader. Some maps appropriately show only one or two pertinent hydrogeologic parameters. Point‐data maps make little or no interpretation of the data. Four‐dimensional maps‐those that include an elapsed span of time or projection of hydrogeologic variables into the future‐represent a high degree of interpretation of data; they...
Flow probability of New Jersey streams
E.G. Miler
1966, New Jersey Division of Water Policy and Supply Water Resources Circular 15
This report is one of a series published by the Division of Water Policy and Supply of the New Jersey Department of Conservation and Economic Development to make basic water data available in a form that can be readily used by all interested persons. The objective of the present report...
Water resources data for Iowa 1966, Part 1--Surface water records
U.S. Geological Survey
1966, Report
No abstract available...
Water resources data for Iowa 1966, Part 2--Water quality records
U.S. Geological Survey
1966, Report
No abstract available...
Water resources data for North Dakota
Water Resources Division, U.S. Geological Survey
1966, Report
No abstract available....
Some Debye temperatures from single-crystal elastic constant data
R. A. Robie, J.L. Edwards
1966, Journal of Applied Physics (37) 2659-2663
The mean velocity of sound has been calculated for 14 crystalline solids by using the best recent values of their single‐crystal elastic stiffness constants. These mean sound velocities have been used to obtain the elastic Debye temperatures θDe for these materials. Models of the three wave velocity surfaces for calcite are illustrated....
Determination of Columbia River flow times from Pasco, Washington using radioactive tracers introduced by the Hanford reactors
Jack L. Nelson, R.W. Perkins, W.L. Haushild
1966, Water Resources Research (2) 31-39
Radioactive tracers introduced into the Columbia River in cooling water from the Hanford reactors were used to measure flow times downstream from Pasco, Washington, as far as Astoria, Oregon. The use of two tracer methods was investigated. One method used the decay of a steady release of Na24 (15-hour half-life)...