M. E. Cooley, J. W. Harshbarger, J. P. Akers, W. F. Hardt, O.N. Hicks
1964, Open-File Report 64-41
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Publication Extents
Not all publications have extents, not all extents are completely accurateAlfred R. Taylor
1964, Geologic Quadrangle 287
John K. Adams, Durward H. Boggess
1964, Hydrologic Atlas 101
D. R. Mabey, M. D. Crittenden Jr., H. T. Morris, R. J. Roberts, E. W. Tooker
1964, Geophysical Investigations Map 422
Frank R. Moore
1964, Open-File Report 64-116
No abstract available. ...
James P. Minard, James Patrick Owens, Thomas C. Nichols
1964, Geologic Quadrangle 272
G.H. Hughes, C. C. McDonald
1964, Open-File Report 64-86
J. H. Morgan
1964, Hydrologic Atlas 113
F.A. Watkins Jr.
1964, Open-File Report 64-159
A. Rice Green
1964, Water Supply Paper 1671
No abstract available....
J. H. Green
1964, Water Supply Paper 1779-T
Ground water in the Southwestern United States is derived chiefly from unconsolidated to semiconsolidated alluvial deposits. Where these deposits contain confined water, they may be susceptible to compaction and related land- surface subsidence, if artesian pressures are reduced. Compaction of artesian-aquifer systems can be estimated from core tests if the...
Roy Lee Griggs, John David Hem
1964, Water Supply Paper 1753
No abstract available....
Robert George Schmidt, William Thomas Pecora, B. C. Hearn Jr.
1964, Bulletin 1141-P
Burdge Irelan
1964, Open-File Report 64-87
John Isbister
1964, Open-File Report 64-88
Benjamin L. Jones
1964, Open-File Report 64-92
Analyses of data collected from two small basins in northern Pennsylvania during the period May 1954-September 1960 indicated a general relationship between changes in land use and land treatment and changes in suspended-sediment discharge from the basins. Extensive land use and land-treatment changes have taken place in the 12.2 square-mile...
J.R. Jones
1964, Open-File Report 64-93
A.M. La Sala Jr., W. E. Harding, R.J. Archer
1964, Open-File Report 64-101
James E. Luzier
1964, Open-File Report 64-107
A water well was drilled recently at the new headquarters site of Mount Rainier National Park, Washington. The headquarters site is in the narrow bedrock-walled, alluvium-floored valley of the Nisqually River. The well was drilled to a depth of 96 feet in a terraced outwash deposit which underlies the site....
M.E. MacLachlan
1964, Open-File Report 64-112
D.G. Metzger
1964, Open-File Report 64-113
G.A. Miller
1964, Open-File Report 64-114
A.M. Moore
1964, Open-File Report 64-115
A.W. Noehre, G.L. Walter
1964, Open-File Report 64-118
William Ogilbee, R.C. Vorhis, Fituri Deghaies
1964, Open-File Report 64-119