William F. Outerbridge
1977, Open-File Report 77-248
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Page 5867, results 146651 - 146675
Publication Extents
Not all publications have extents, not all extents are completely accurateGary W. Hill, Ralph Eugene Hunter
1977, Open-File Report 77-98
No abstract available....
Victoria R. Todd
1977, Open-File Report 77-742
No abstract available....
Jerry L. Hughes
1977, Water-Resources Investigations Report 76-128
The quality and quantity of recharge to the Santa Maria Valley groundwater basin from natural sources, point sources, and agriculture were evaluated. The results are expressed in terms of a hydrologic budget, a solute balance, and maps showing the distribution of selected chemical constituents in ground water. Point sources of...
Helen M. Beikman, C. D. Holloway, E. M. MacKevett
1977, Open-File Report 77-169-B
No abstract available....
A. F. Bateman Jr., G. A. Lutz
1977, IMAP 1013
No abstract available....
Andrew F. Bateman Jr., L. A. Shoaff, Terry R. Flot
1977, Open-File Report 77-626
No abstract available....
T.W. Dibblee Jr.
1977, Open-File Report 77-611
Carleen D. Holloway
1977, Open-File Report 77-169-D
No abstract available....
E. Neal Hinrichs
1977, Open-File Report 77-620
Richard L. Reynolds
1977, Open-File Report 77-355
Detrital grains of the rhombohedral ilmenite (FeT1O3)--hematite (Fe2O3) solid solution series (titanohematites) have been identified by thermomagnetic, reflection microscopic, and X-ray diffraction analysis in six uranium-bearing sandstones in the western United States. Many of the titanohematites are ferrimagnetic and have Curie temperatures ranging from about 70 Deg C to 220...
Wayne L. Newell, C. L. Rice
1977, Miscellaneous Field Studies Map 865-C
No abstract available....
G. A. Payne
1977, Open-File Report 77-424
Long Meadow Lake, Black Dog Creek, and Ponds AP-9 and AP-10 which lie in an area designated for a trunk highway bridge crossing the Minnesota River, were sampled for baseline water quality prior to construction of the bridge. Data collected show that dissolved solids fluctuate seasonally. Dissolved oxygen:/ranged from less...
Donald L. Peterson, Harold E. Kaufmann
1977, Open-File Report 77-67-D
Kim Manley
1977, Miscellaneous Field Studies Map 877
B. A. Kososki, A. G. McHendrie, J. B. Baker
1977, Miscellaneous Field Studies Map 852
No abstract available....
D. R. Nichols, N. A. Wright
1977, Miscellaneous Field Studies Map 891
No abstract available....
Wayne L. Newell
1977, Miscellaneous Field Studies Map 843
Wayne L. Newell
1977, Miscellaneous Field Studies Map 844
Water Resources Division, U.S. Geological Survey
1977, Professional Paper 1050
No abstract available....
D.E. Funderburg
1977, Open-File Report 77-261
The U.S. Geological Survey, in cooperation with the U.S. Soil Conservation Service, began an investigation of sedimentation of Bernalillo Floodwater Retarding Reservoir No. 1 (Piedra Lisa Arroyo) near Bernalillo, New Mexico in 1956. This investigation was part of a nationwide investigation of the trap efficiency of detention reservoirs. Reservoirs No....
Gary S. Fuis, Carl E. Johnson, D.J. Jenkins
1977, Open-File Report 77-869
The northern section of the Imperial Valley region in southern California is an area of known geothermal resources and an area of high seismicity. To study in detail the relationship between geothermal areas and earthquakes, the U.S. Geological Survey has been monitoring seismicity in the Imperial Valley with a 16...
G. W. Levings, C. D. Farrar
1977, Water-Resources Investigations Report 77-50
The southern part of the Chinle area includes about 2,100 sq mi in northeastern Arizona and is entirely in the Navajo Indian Reservation. The main source of water is the ground water in the several aquifers that are made up of one or more formations. The aquifers are stacked one...
Water Resources Division, U.S. Geological Survey
1977, Open-File Report 77-62
John E. Hull, T.R. Beaven
1977, Open-File Report 77-803
During the 1975 calendar year rainfall in Dade County, Fla., was 14.89 inches below the long-term average (57.17 in.). Ground-water levels ranged from 0.1 foot above to 1.1 feet below average. The highest and lowest ground-water levels for the year were both 1 foot below their long-term averages. In the...