S. G. Robson, F.W. Glessner
1966, Open-File Report 66-115
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Publication Extents
Not all publications have extents, not all extents are completely accurateGeorge M. Farlekas
1966, Open-File Report 66-43
A stream overflowing its banks is a natural phenomenon. This natural phenomenon of flooding has occurred on the Delaware River in the past and will occur in the future. T' o resulting inundation of large areas can cause property damage, business losses and possible loss of life, and may result...
R. A. Robie, P. M. Bethke, Keith Beardsley
1966, Open-File Report 66-113
F. S. Riley
1966, Open-File Report 66-111
Arthur Johnson
1966, Open-File Report 66-68
H. T. Hopkins
1966, Open-File Report 66-63
No abstract available. ...
T.J. Irza
1966, Open-File Report 66-67
Preliminary flood-frequency relations have been defined for small streams in Kansas for floods having recurrence intervals not greater than 10 years. The defined relations will be useful for the design of culverts and other hydraulic structures. The relations are expressed in terms of basin characteristics.Peakflow records at 95 sites in...
J.A. Bettendorf
1966, Open-File Report 66-6
R.F. Norvitch, M.E.S. Lamb
1966, Open-File Report 66-93
L.S. Hughes
1966, Open-File Report 66-64
No abstract available....
R. M. Bloyd Jr.
1966, Open-File Report 66-7
This progress report presents the results of a test-well drilling program undertaken by the Antelope Valley-East Kern Water Agency and the U.S. Geological Survey in the western part of Antelope Valley, Calif. Eight test wells were drilled by the rotary method, and electric and lithologic logs were made of each...
S.M. Lang, A.R. Leonard
1966, Open-File Report 65-95
Bernard Dunn
1966, Open-File Report 66-30
R. L. Knutilla
1966, Open-File Report 66-72
Rafael Perez Siliceo, David Gallagher
1966, Open-File Report 66-124
R. H. Dale, James J. French, G. V. Gordon
1966, Open-File Report 66-21
The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the 700,000 acre-feet per year flow of...
Deric O’Bryan
1966, Open-File Report 66-94
J. R. Wall, E. H. Cordes, J. A. Moreland
1966, Open-File Report 66-151
David L. Durham
1966, Open-File Report 66-33
C.E. Shaw Jr.
1966, Open-File Report 66-123
No abstract available....
Robert G. Dickinson
1966, Open-File Report 66-24
The Cerro Summit quadrangle covers 58 square miles of dissected plateau on the south flank of the Gunnison uplift in southwestern Colorado. It lies east of the Uncompahgre River valley and south of the Black Canyon of the Gunnison River. Rocks dip gently in most of the quadrangle, but they...
S.M. Lang, A.R. Leonard
1966, Open-File Report 66-76
Robert Hadley Moench, Avery Drake Jr.
1966, Open-File Report 66-87
The Idaho Springs mining district forms an important segment of the Front Range mineral belt, a northeast-trending zone of coextensive intrusive rocks and hydrothermal ore deposits of early Tertiary age. This belt, which is about 50 miles long, extends from the region just west of Boulder southwestward across the Front...
J.S. Rosenshein
1966, Open-File Report 66-118
S. L. Johnson
1966, Open-File Report 72-198
No abstract available....