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Page 5757, results 143901 - 143925

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Not all publications have extents, not all extents are completely accurate
Geothermal potential of the Dieng Mountains, Central Java, Indonesia
L.J. Patrick Muffler
1970, Open-File Report 70-236
This report summarizes results of a 2-week (Feb. 23-Mar. 10, 1970) study of the geothermal resources of the Dieng Mountains, Java; the work was done as part of a cooperative program of the Ministry of Mines and the U. S. Geological Survey under the auspices of the Government of Indonesia...
Floods in the upper Des Moines River Basin, Iowa
Harlan H. Schwab
1970, Open-File Report 70-296
Data on flood stages, discharges, and frequency are used in the design of bridges and other structures and the conduct of various operations on the flood plains of streams. This report provides these data in the form of flood-peak records, gaging-station records, frequency curves, and flood profiles. Information is provided...
Determination of the manning coefficient from measured bed roughness in natural channels
John Thomas Limerinos
1970, Water Supply Paper 1898-B
This report presents the results of a study to test the hypothesis that basic values of the Manning roughness coefficient of stream channels may be related to (1) some characteristic size of the streambed particles and to (2) the distribution of particle size. These two elements involving particle size can...
Elemental sulfur in Eddy County, New Mexico
Jim S. Hinds, Richard R. Cunningham
1970, Circular 628
Sulfur has been reported in Eddy County, N. Mex., in rocks ranging from Silurian to Holocene in age at depths of 0-15,020 feet. Targets of present exploration are Permian formations in the Delaware Basin and northwest shelf areas at depths of less than 4,000 feet. Most of the reported sulfur...
Water resources of the Wild Rice River watershed, northwestern Minnesota
Thomas C. Winter, L. E. Bidwell, Robert W. Maclay
1970, Hydrologic Atlas 339
The Wild Rice watershed includes two general physiographic areas- the glacial Lake Agassiz Plain and a glacial moraine. The lake plain is extremely flat in the western part, sloping only a few feet per mile, but in the eastern part the plain is traversed in a north-south direction by long, narrow...
Analyses of stream-sediment samples from western St. Lawrence Island, Alaska
William Wallace Patton Jr., Bela Csejtey Jr.
1970, Open-File Report 70-258
Analytical data for 207 stream-sediment samples from western St. Lawrence Island are presented in this report, together with a statistical treatment of the data. The samples were collected in 1968 and 1969 as part of the Heavy Metals Program of the U.S. Geological Survey.This report is intended to supplement Geological...