J. R. Balsley Jr., M. E. Hill, J. L. Meuschke
1951, Geophysical Investigations Map 48
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateP.K. Sims, Preston Enslow Hotz
1951, Bulletin 978-D
John R. Henderson Jr., J. L. Meuschke
1951, Geophysical Investigations Map 86
No abstract available....
J. R. Balsley Jr., M. E. Hill, J. L. Meuschke
1951, Geophysical Investigations Map 46
No abstract available....
James F. Pepper, Wallace De Witt Jr.
1951, Oil and Gas Investigation Chart 45
Water Resources Division, U.S. Geological Survey
1951, Water Supply Paper 1123
Mortimer Hay Staatz, Herman L. Bauer Jr.
1951, Circular 142
The Virgin Valley opal district, Humboldt County, Nevada, is near the Oregon-Nevada border in the Sheldon Game Refuge. Nineteen claims owned by Jack and Toni Crane were examined, sampled, and tested radiometrically for uranium. Numerous discontinuous layers of opal are interbedded with a gently-dipping series of vitric tuff and ash...
John J. Matzko
1951, Trace Elements Investigations 45-C
Robert M. Lindvall
1951, Open-File Report 51-71
C.L. Jacobsen, E. W. Reed
1951, Open-File Report 51-121
No abstract available....
N.D. Hoy
1951, Open-File Report 51-118
No abstract available....
H. E. Thomas
1951, Open-File Report 51-153
P.D. Akin
1951, Open-File Report 51-91
The Mohall area includes about 120 square miles in Bottineau and Renville Counties in northwestern North Dakota. Mohall, whose 1950 population was 1,073, is the only town in the area. The area is part of the Drift Prairie section of the Central Lowland physiographic province. It is characterized by the...
R.W. Stallman, R. H. Brown
1951, Open-File Report 51-150
No abstract available....
F.D. Trauger
1951, Open-File Report 51-155
The Baker Valley is the southern part of a small oval-shaped inter-montane structural basin located near tie southeastern edge of the Blue Mountains of northeastern Oregon. The Powder River enters and leaves the valley through narrow rock gorges. The alluviated basin floor at an altitude of about 3,400 feet is...
H. E. LeGrand, G.E. Siple
1951, Open-File Report 51-125
E.D. Gordon, R.J. Dingman
1951, Open-File Report 51-111
C.A. Repenning, L.C. Halpenny, J.A. Hem
1951, Open-File Report 51-143
The ground-water resources of the Keams Canyon area were investigated by the Ground Water Branch of the United States Geological Survey in the fall of 1949 and the spring of 1950. The area lies between latitudes 35o30', and 36o00', and between longitudes 110o00' and 110o15', in the Hopi Indian Reservation,...
R. C. Newcomb
1951, Open-File Report 51-35
Donald George Metzger
1951, Open-File Report 51-28
The Ranegras Plain area is part of the Basin and Range province in west-central Arizona. The report discusses rocks of pre-Cambrian, pre-Cambrian (?), Paleozoic (?), Mesozoic (?), Cretaceous (?), Cretaceous and Tertiary, Tertiary (?), Quaternary (?), and Quaternary age. All the Paleozoic (?) and Cretaceous (?) rocks and parts of the...
Fred C. Mickels, Porter E. Ward
1951, Open-File Report 51-138
The City of Evansville, Ind. has utilized the Ohio River as a source of municipal water supply for many years. The average daily pumpage for the city in 1950 was reported to be about 18.5 million gallons. Because of the extreme variability in the quality of the river water and the...
C. L. McGuinness
1951, Open-File Report 51-137
No abstract available. ...
C. L. McGuinness
1951, Open-File Report 51-136
No abstract available....
N.J. Lusczynski, J.F. Hoffman
1951, Open-File Report 51-135
No abstract available....
N.J. Lusczynski
1951, Open-File Report 51-131
This report presents and discusses the quantitative and qualitative data obtained during a pumping test at the Levittown housing development in Nassau County, N. Y. One of the ten principal supply wells, screened in the sands of the Magothy (?) formation which is overlain unconformably by the sand and gravel...