Robert W. Maclay, James E. Heisel
1972, Open-File Report 72-243
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Publication Extents
Not all publications have extents, not all extents are completely accurateWillard B. Mills
1972, Open-File Report 72-257
The U.S. Geological Survey, in cooperation with the Sabine River Compact Administration, conducted time-of-travel studies in the Sabine River Basin on April 16-30, 1972. One study was made on the main stem of the Sabine River in four reaches from Lake Tawakoni to Toledo Bend Reservoir, a distance of 219...
D.W. Moody, Olaf Kays
1972, Open-File Report 72-260
The Generalized Information Processing System (GIPSY) stores and retrieves variable-field, variable-length records consisting of numeric data, textual data, or codes. A particularly noteworthy feature of GIPSY is its ability to search records for words, word stems, prefixes, and suffixes as well as for numeric values. Moreover, retrieved records may be...
A. B. Gibbons
1972, Geologic Quadrangle 1025
John R. Ritter, William M. Brown III
1972, Open-File Report 72-315
Fifty-two acre-feet of sediment was ·deposited in Williams Reservoir between 1913 and 1971. From calculations of the sediment yields in other nearby drainage basins in Santa Clara County, it was determined that 24 to 38 acre-feet of sediment would have been transported to Williams Reservoir between 1961 and 1971 under...
Calvin Stanton Bromfield, Frank E. Williams, Peter Popenoe
1972, Bulletin 1353-A
No abstract available....
Stanley G. Robson
1972, Open-File Report 72-320
The Saugus-Newhall area is in the upper Santa Clara River valley, in northwestern Los Angeles. County, about 30 miles north of Los Angeles. The area has two main aquifers, the alluvial aquifer and the underlying Saugus aquifer. These two aquifers are the subject of this investigation. The alluvial aquifer consists...
Charles W. Sever
1972, Open-File Report 72-345
Aquifer-performance tests and aquifer studies indicate that the limestone beneath the city of Adel and probably most of Cook County contains potable water to a depth of only about 400 to 500 feet and that "deep" wells that tap these limestones obtain most of their water from a few thin,...
Water Resources Division, U.S. Geological Survey
1972, IMAP 784-R
No abstract available....
Water Resources Division, U.S. Geological Survey
1972, Water Data Report OK-71-2
No abstract available....
Kenneth John Englund, John F. Windolph Jr.
1972, Open-File Report 72-113
Donald L. Peterson
1972, Open-File Report 72-297
No abstract available. ...
1972, Miscellaneous Field Studies Map 440
No abstract available. ...
E. H. Cobb
1972, Miscellaneous Field Studies Map 393
C. L. Hummel, Hashim Hakim
1972, Open-File Report 72-179
1972, Miscellaneous Field Studies Map 445
No abstract available. ...
Arden Leroy Albee, Eugene L. Boudette, John W. Allingham
1972, Bulletin 1297
No abstract available....
Water Resources Division, U.S. Geological Survey
1972, Water Data Report PA-71-1
No abstract available. ...
Maurice A. Chaffee
1972, Open-File Report 72-65
No abstract available....
William E. Bowers
1972, Bulletin 1331-B
1972, Miscellaneous Field Studies Map 374
No abstract available....
K. A. Howard
1972, Open-File Report 72-170
No abstract available. ...
Arnold Leslie Brokaw
1972, Open-File Report 72-49
No abstract available....
Water Resources Division, U.S. Geological Survey
1972, Professional Paper 800-A
No abstract available....
Robert Sprague Jones
1972, Open-File Report 72-200
Geologic and radiometric studies and chemical analyses of soils, rocks, and water were made north of an area between Edgemont and Hot Springs, South Dakota.The soil is shallow, poorly developed, and not present in some areas. The median pH of the soil from three areas ranges from 6.7 to 7.0....