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Page 1837, results 45901 - 45925

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Aquifer-test compilation for the San Joaquin Valley, California
E.J. McClelland
1962, Open-File Report 62-80
This report is the first of a series the purpose of which is to make available in standard tabular form the results of aquifer tests that have been made by various private and public agencies in California. The scope of the compilation is to describe systematically, in a form agreed...
Ground-water reconnaissance in Round Valley, Custer County, Idaho
E. G. Crosthwaite
1962, Open-File Report 62-33
Round Valley in central Idaho contains alluvial deposits of Pleistocene and Recent age which yield adequate supplies of ground water for stock and domestic wells. The alluvial deposits are underlain by Challis Volcanics of Oligocene or Early Miocene age and a few wells obtain domestic and stock water from the...
Mercury in the United States, exclusive of Alaska and Hawaii
Edgar Herbert Bailey
1962, Mineral Investigations Resource Map 30
This map shows the location of mercury districts and deposits in the United States (exclusive of Alaska and Hawaii). The map was compiled from published reports and from data in the files of the Geological Survey. All map locations are numbered consecutively in each state and names, geographic coordinates, and...
Bismuth in the United States, exclusive of Alaska and Hawaii
John Roberts Cooper
1962, Mineral Investigations Resource Map 22
The bismuth-bearing deposits in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. In compiling the map the deposits were classified into two categories: 1) those that have produced bismuth or are regarded as potential sources based on available information (in general, this category includes...
Titanium in the United States, exclusive of Alaska and Hawaii
Cleaves Lincoln Rogers, Marion Charlotte Jaster
1962, Mineral Investigations Resource Map 29
The accompanying map shows the location of the principal deposits of titanium minerals in the United States (excluding Alaska and Hawaii). Four broad geologic categories of deposits have been distinguished on the map by the shapes of the symbols, and relative importance is indicated by their size. The smaller deposits...
An application of thermometry to the study of ground water
Robert Schneider
1962, Water Supply Paper 1544-B
Except for studies of temperature data related to ground-water developments that induce infiltration from streams, little attention has been given to the possibility of using temperature fluctuations as a tool for studying the elements of the hydrologic cycle involving ground water. The temperature of the water discharged from large installations that...
Methods of measuring soil moisture in the field
A.I. Johnson
1962, Water Supply Paper 1619-U
For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. Much equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses...
Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60
Kerry F. Harris
1962, Water Supply Paper 1547
This inventory of published and unpublished sediment-load data contains a list of the sediment-transport measurements in the United States and Puerto Rico during October 1950 to September 1960, made by the agencies associated with the Subcommittee on Sedimentation. Some of the agencies have miscellaneous sediment data, such as single observations...
Beryllium in the United States, exclusive of Alaska and Hawaii
Wallace R. Griffitts, David Marcel Larrabee, James Jennings Norton
1962, Mineral Investigations Resource Map 35
This map shows most of the known occurrences of beryllium minerals and of rocks that contain 0.003 percent or more beryllium (0.01 percent Be0) in the United States (exclusive of Alaska and Hawaii). The occurrences are subdivided on the map according to genesis and size. The genetic types of deposits...
Lower Ipswich River basin
Edward A. Sammel, John A. Baker
1962, Ground-water Series 2
The lower Ipswich River basin is that part of the Ipswich River drainage basin below the Geological Survey stream-gaging station at South Middleton in northeastern Massachusetts (fig. 1). It includes about 110 square miles between the gaging station at South Middleton and the Atlantic Ocean. This report presents basic data collected...
Surface water records of Indiana, 1962
Water Resources Division, U.S. Geological Survey
1962, Report
The surface-water records for the 1962 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
Thermodynamic properties of minerals
Richard A. Robie
1962, Trace Elements Investigations 816
In the ten years since the publication of the national Bureau of Standards comprehensive tables of thermochemical properties, by Rossini and other (1952), a very large body of modern calorimetric and equilibrium data has become available. Because of the complex interrelations among many thermochemical data and the necessity for internal...
Stability relations of the ferruginous biotite, annite
H.P. Eugster, D. R. Wones
1962, Journal of Petrology (3) 82-125
Annite, KFe3AISi3O10(OH)2 a member of the iron biotites and the ferrous analogue of phlogopite, has been synthesized and its phase relations have been determined as functions of temperature, fugacity of oxygen (fo2), and total pressure (Ptotal≈PH2O+PH2). A method for controlling fo2at high total pressures is described, and data for the 'oxygen...
Remanent magnetism as a contributor to some aeromagnetic anomalies
K. G. Books
1962, Geophysics (27) 359-375
An investigation of some aeromagnetic anomalies in north-central Montana shows that remanent magnetization is the dominant factor in anomalies over some rocks and a contributing factor in anomalies over others. In volcanic rocks, remanence is commonly south-seeking down and has an intensity approximately ten times the induced intensity of magnetization. Remanence is shown to be...
Perspective on problems of hydrogeology
H. E. LeGrand
1962, Geological Society of America Bulletin (73) 1147-1152
A trend toward increasing use of test drilling and subsurface exploration is resulting in a decreasing reliance on human experience in coping with problems in hydrogeology. Application of "observation and inference" and discreet abstraction of readily available data will solve more problems than is now realized. ...
Statistical properties of tree ring data
N.C. Matalas
1962, International Association of Scientific Hydrology - Bulletin (7) 39-47
A statistical analysis is made of the sequences of annual tree ring widths and indices. The expected value of growth during any year is shown to be proportional to the standard deviation of the growth, so that the coefficient of variation is a measure of the sensitivity of the growth of a <span...
Limiting parameters in the magnetic interpretation of a geologic structure
G. E. Andreasen, I. Zietz
1962, Geophysics (27) 807-814
A prominent aeromagnetic anomaly in Randolph County, Indiana, suggests the existence of a dikelike structure within the Precambrian basement rocks. Because of the ambiguity inherent in magnetic interpretation, a unique solution for the parameters involved (depth of burial, geometric configuration, and magnetic susceptibility of the mass producing the anomaly) is impossible. However, if one of the <span...
Records of wells and ground-water quality in Burlington County, New Jersey
F. Eugene Rush
1962, Report
<This basic-data report is limited to the presentation of selected drillers' logs and their geologic correlations, well data, and chemical analyses of water from wells in Burlington County, N. J. The county lies within the Coastal Plain province; it is underlain by unconsolidated sediments of Quarternary, Tertiary, and Cretaceous...