Preliminary digital model studies of the Rio Aconcagua Valley, Chile
O. James Taylor
1970, Open-File Report 71-278
A land use interpretation experiment, TR 69-5
Nelson R. Nunnally, Richard E. Witmer
1970, Open-File Report 71-218
Principal facts for gravity stations in Howard County, Maryland
John Wing Allingham
1970, Open-File Report 70-4
Approximate optimum yield of the glacial outwash aquifer between Sioux Falls and Dell Rapids, South Dakota
J.E. Powell, D. G. Jorgensen
1970, Open-File Report 71-228
No abstract available....
Ground-water conditions in the central Virgin River basin, Utah - A progress report for 1968-69
R.M. Cardova, G. W. Sandberg, Wilson McConkie
1970, Open-File Report 70-55
No abstract available....
Aeromagnetic map of the Quabbin Reservoir quadrangle, Franklin, Worcester, and Hampshire Counties, Massachusetts
Water Resources Division, U.S. Geological Survey
1970, Geophysical Investigations Map 698
Sedimentation in Third Creek Subwatershed No. 7A, North Carolina
Howard E. Reeder
1970, Open-File Report 71-235
Chemical analyses of rock and soil samples from the Chandalar and eastern Wiseman quadrangles, Alaska
William Peters Brosge, H. N. Reiser
1970, Open-File Report 70-39
No abstract available....
Chemical quality of Michigan streams
Warren W. Wood
1970, Circular 634
Concentrations of chemical constituents of Michigan streams exhibit regional patterns that are primarily a function of geology and evapotranspiration. However, in some areas waste disposal by municipal and industrial organizations has altered the natural distribution and concentrations of dissolved material. Concentration and areal distribution of chemical constitutents were found to...
Results of geochemical sampling in the western Clearwater Mountains, Alaska
Thomas E. Smith
1970, Open-File Report 70-310
Two centers of gold mineralization in the Clearwater Mountains have been identified during a recent geochemical sampling program in the Healy A-1, B-1 quadrangles, Alaska. Both the Timberline Creek center and the Black Creek center are located near the same E-W trending fault system.Sites of structural weakness along the zone...
A preliminary study of the effects of water circulation in the San Francisco Bay estuary : A. Some effects of fresh-water inflow on the flushing of south San Francisco Bay, B. Movement of seabed drifters in the San Francisco Bay estuary and the adjacent Pacific Ocean
D. S. McCulloch, D. H. Peterson, P.R. Carlson, T. J. Conomos
1970, Circular 637-A,B
Structural geology of the Wind River Basin, Wyoming
W. R. Keefer
1970, Professional Paper 495-D
Water as an urban resource and nuisance
H. E. Thomas, William Joseph Schneider
1970, Circular 601-D
Generally, when people speak of water as a resource, they are considering its good aspects and recognizing that it is essential for life and living. Sometimes or at some places or to some people, the same water may be annoying or unpleasant and thus a nuisance-for example, rain at a...
A proposed streamflow-data program in Alaska
J.M. Childers
1970, Open-File Report 70-62
The streamflow-data program in Alaska was analyzed to design a better data network. The analysis included (1) definition of the goals of the streamflow-data program, (2) evaluation of the available data to see which goals have already been achieved, and (3) consideration and recommendation of future programs to achieve the...
Stream dispersion at selected sites
R.G. Godfrey, B. J. Frederick
1970, Professional Paper 433-K
Geohydrologic significance of lithofacies of the Cockfield Formation of Louisiana and Mississippi and of the Yegua Formation of Texas
J.N. Payne
1970, Professional Paper 569-B
No abstract available....
Report on field trip to Wadi Bidah and Ablah areas, Saudi Arabia
Louis Gonzalez
1970, Open-File Report 70-138
The Mulgatah ancient workings were briefly examined and two samples of alluvium were taken from the wadi that drains these workings. In Wadi Bidah, near gossan outcrops at the Rabathan prospects, another wadi sample was taken. In the Abla Formation area, seven wadi samples were taken and these samples as...
Preliminary geologic map of the Wilhelm quadrangle of the Moon
Ronald Stephen Saunders
1970, Open-File Report 70-286
Results of analyses for shale oil in the Phosphoria Formation of southwestern Montana
Andrew F. Bateman Jr.
1970, Open-File Report 70-19
Atlantic Continental Shelf and Slope of the United States - Gravels of the northeastern part
John Schlee, R. M. Pratt
1970, Professional Paper 529-H
Maps showing locations of holes drilled in 1953 to 1955 by U.S. Geological Survey, Deer Flat and adjacent areas, San Juan County, Utah
Tommy Lee Finnell, P.C. Franks, O.T. Marsh, D. A. Brew
1970, Open-File Report 70-123
Preliminary evaluation of chemical and biological characteristics of the upper St. Johns River basin, Florida
D. A. Goolsby, B. F. McPherson
1970, Open-File Report 71-124
Seismic activity in the Sunnyside mining district, Carbon and Emery Counties, Utah, during 1968
C. Richard Dunrud, John O. Maberry, Jerome H. Hernandez
1970, Open-File Report 70-115
More than 20,000 local earth tremors were recorded by the seismic monitoring network in the Sunnyside mining district during 1968. This is about 40 percent of the number of tremors recorded by the network in 1967. In 1968 a total of 281 tremors were of sufficient magnitude to be located...
A proposed streamflow data program for South Carolina
Jeffrey T. Armbruster
1970, Open-File Report 70-11
An evaluation of the available streamflow data in South Carolina was made to provide guidelines for planning future surface-water data programs. The basic elements in the evaluation procedure were (1) establishment of objectives and goals of the program, (2) examination and analysis of all available data to determine which goals...
Geology and mineral evaluation of the Wadi Bidah district, southern Hijaz quadrangle, Kingdom of Saudi Arabia
Robert L. Earhart, Mustafa M. Mawad
1970, Open-File Report 70-116
The Wadi Bidah district in southwest Saudi Arabia contains several ancient mines and mineral-prospects. The Precambian rocks of the district are steeply dipping and highly folded and faulted. They are divided into three major units: (1) older metavolcanic rocks, (2) metasedimentary rocks, and (3) younger metavolcanic rocks. Massive sulfide-type deposits...