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Page 6385, results 159601 - 159625

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Ground water available in the Davenport area, Oklahoma
Stuart L. Schoff
1948, Open-File Report 48-83
This memorandum describes the ground-water resources in the vicinity of Davenport, Lincoln County, Oklahoma. It is based on a one-day trip to Davenport made by the writer on February 11, 1948, to obtain information in addition to that in the ground-water files in Norman on the availability of ground water...
Discharge and runoff in the Missouri River basin
Bruce R. Colby, Roy E. Oltman
1948, Circular 37
Within the Missouri River Basin the precipitation and temperature vary greatly with both time and geographical location. Differences in weather and climate combine with differences in topography and geology to produce large differences in runoff from time to time and from place to place in the basin. The average annual...
Gold deposits of the southern Piedmont
J. T. Pardee, C. F. Park Jr.
1948, Professional Paper 213
This report deals chiefly with the gold mines in the Southern Appalachian gold belt whose workings were accessible at the time of examination, but it also · summarizes available information concerning many mines that were not accessible. Most of the mines lie within a belt, 10 to 100 miles wide,...
Tests and researches on building stones
M. R. L’Hermite
1948, Open-File Report 48-17-E
In 1941, the "Association Francaise de Normalisation" (French Association of Standardization) decided to create a Commission for the purpose of writing out a standard for building stones. When this Commission met under the chairmanship of Mr. Pol Abraham, Architect, they realized how far behind was our precise technical knowledge of...
Special problem caused by the epigenetic alterations of Liassic rocks
Henry Joly, Ninck Joly
1948, Open-File Report 48-17-B
"Special problem caused by the epigenetic alterations of Liassic rocks", by Henry Joly and Ninck, describes damages to the foundation of a building in Nancy due to swelling of a Jurassic shale bed. The swelling was due to the formation of calcium sulphate by chemical reaction of constituents of the...