Harold Lloyd James
1962, Open-File Report 62-65
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Page 6062, results 151526 - 151550
Publication Extents
Not all publications have extents, not all extents are completely accurateDaniel R. Shawe, George Clarke Simmons, Norbert Lee Archbold
1962, Open-File Report 62-125
No abstract available....
J. W. Hood, Lester Ray Kister
1962, Water Supply Paper 1601
No abstract available....
Water Resources Division, U.S. Geological Survey
1962, Professional Paper 450-A
Irwin Remson, J.R. Randolph
1962, Professional Paper 411-D
Robert Francis Johnson
1962, Bulletin 1110-A
E. Neal Hinrichs, E. J. McKay
1962, Open-File Report 62-61
Luna Bergere Leopold
1962, Circular 460-A
He was sitting on a large slab of rock. As he looked at the cloud of dust hanging hazily on the horizon, the piece of antler and the block of flint he held in his hand hung as if they were suspended from their previous rapid motion. The man gazed...
Arnold Leslie Brokaw, G. B. Gott, D. R. Mabey, Howard McCarthy, Uteana Oda
1962, Circular 475
No abstract available....
F. H. Olmsted, A. G. Hely
1962, Professional Paper 417-A
The relation between ground water and surface water was studied in Brandywine Creek basin, an area of 287 square miles in the Piedmont physiographic province in southeastern Pennsylvania. Most of the basin is underlain by crystalline rocks that yield only small to moderate supplies of water to wells, but the...
W. B. Langbein
1962, Water Supply Paper 1539-W
Charles William Carlston
1962, Bulletin 1141-I
E. G. Crosthwaite
1962, Open-File Report 62-33
Round Valley in central Idaho contains alluvial deposits of Pleistocene and Recent age which yield adequate supplies of ground water for stock and domestic wells. The alluvial deposits are underlain by Challis Volcanics of Oligocene or Early Miocene age and a few wells obtain domestic and stock water from the...
J. L. Meuschke, P. W. Philbin, F.A. Petrafeso
1962, Geophysical Investigations Map 304
No abstract available....
I. Wendell Marine
1962, Water Supply Paper 1475-G
A water supply of 50 gpm (gallons per minute) is estimated to be sufficient to supply the present and future water demand at the monument. The Coconino sandstone of Permian age seems to be capable of yielding this quantity to a well between 1,500 and 2,700 feet deep in the...
G. E. Andreasen, F. C. Smith
1962, Geophysical Investigations Map 340
G.M. Richmond
1962, Professional Paper 324
John R. Donnell
1962, Open-File Report 62-38
No abstract available....
J. S. Meyers, T. J. Nordenson
1962, Professional Paper 272-D
No abstract available....
G. E. Harbeck Jr.
1962, Professional Paper 272-E
Studies of evaporation made in recent years nave provided values of the mass-transfer coefficient, N, in the equation E=Nut(e0—ea) for reservoirs having surface areas ranging from 1 to nearly 30,000 acres. The apparent correlation of N with reservoir surface area may in large part be associated with variations in the...
H. T. Morris
1962, Open-File Report 62-89
No abstract available....
E. G. Crosthwaite
1962, Open-File Report 62-34
This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury...
Edward Bradley
1962, Open-File Report 62-10
Howard R. Smith
1962, Oil and Gas Investigation Map 211
No abstract available....
Alexander A. Wanek
1962, Oil and Gas Investigation Map 208
No abstract available. ...