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Page 6150, results 153726 - 153750

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Water and the conservation movement
Luna Bergere Leopold
1958, Circular 402
Every age has its unique touchstone, its hallmark. The Nineties were thought gay. The Twenties had jazz and John Held, Jr. The Thirties had breadlines, dust bowls, the forgotten man. And each recent period has been studded with so many flashy gems, both paste and genuine, that no hallmark would...
Hydraulic and hydrologic aspects of flood-plain planning
Sulo Werner Wiitala, Karl R. Jetter, Alan J. Sommerville
1958, Open-File Report 58-109
The valid incentives compelling occupation of the flood plain, up to and even into the stream channel, undoubtedly have contributed greatly to the development of the country. But the result has been a heritage of flood disaster, suffering, and enormous costs.Flood destruction awakened a consciousness toward reduction and elimination of...
Origin of manganese deposits of Busuanga Island, Philippines
Ronald Keith Sorem
1958, Open-File Report 58-98
The manganese deposits of Busuanga Island, Palawan, are tabular and broadly lenticular bodies which lie conformably within a thick sequence of deformed abort beds. The purpose of this study is to determine the probable mode of origin of the deposits. Similar deposits in other parts of the world have been...
Reconnaissance petrography of the Idaho batholith in Valley County, Idaho
Dwight Lyman Schmidt
1958, Open-File Report 58-89
The purpose of this report is to describe the rocks comprising a part of the Idaho batholith in west-central Idaho (see index map, Figure 1). The study is a by-product of an investigation of placer deposits containing radioactive minerals, monazite and euxenite, by the U. S. Geological Survey on behalf...
Core logs from five holes near Kramer, in the Mojave Desert, California
William K. Benda, Richard C. Erd, Ward C. Smith
1958, Open-File Report 58-12
In 1957, five test holes were drilled near Kramer, California, in =he western Mojave Desert. The drill sites are in topographic basins where gravimetric and geologic surveys indicated the presence, beneath alluvium, of a thick section of Quaternary and Tertiary sedimentary and volcanic rocks. Two holes which were deeper tests...
Reconnaissance for radioactive rocks in the Paulo Afonso Region, Bahia, Brazil
Donald D. Haynes, Henry Mau
1958, Trace Elements Memorandum 1104
Ground and air traverses were made to the northwest, north and northeast of Paulo Afonso, Bahia, Brazil, covering Precambrian crystalline rocks and sedimentary rocks of the Jatoba series of Jurassic or Cretaceous age. No important radioactivity anomalies were found; samples from the two strongest anomalies had an equivalent uranium-oxide content...
Photogeological map of the Flat Top Moutain NE quadrangle Carbon County, Wyoming
A. B. Olson
1958, Trace Elements Memorandum 985
Flat Top Mountain NE quadrangle is on the eastern rim ot the Washakie Basin. The Wasatch and Green River formations crop out in the map area and dip generally to the west. The even and persistent bedding of the Green River formation, combined with the strong benching of a few...
Areal geology of the Little Cone quadrangle, Colorado
Alfred Lerner Bush, O.T. Marsh, Richard Bartlett Taylor
1958, Trace Elements Investigations 602
The Little Cone quadrangle includes an area of about 59 square miles in eastern San Miguel County in southwestern Colorado. It lies within and adjacent to the northeastern boundary of the Colorado Plateau physiographic province. The precipitous front of the San Juan Mountains lies a few miles to the east...
Physical properties of salt, anhydrite and gypsum : preliminary report
Eugene C. Robertson, Richard A. Robie, Kenneth G. Books
1958, Trace Elements Memorandum 1048
This summary is the result of a search of the available literature. Emphasis is placed on the mechanical and calorimetric properties of salt; the measurements of elastic, thermal, magnetic, and mass properties of salt are merely tabulated. Under hydrostatic pressure < 1,000 kg/cm2 at room temperature, salt deforms plastically to...