W.E. Forrest, P. R. Speer
1962, Open-File Report 62-47
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Publication Extents
Not all publications have extents, not all extents are completely accurateW.L. Emerick, D.D. Dickey, C. M. Bunker
1962, Open-File Report 62-40
L.J. Snell
1962, Open-File Report 73-268
Bruce Bryant
1962, Bulletin 1121-D
No abstract available....
R. E. Evenson, H.B. Wilson Jr., K. S. Muir
1962, Open-File Report 62-45
W.S. Twenhofel, R.A. Black, D.F. Balsinger
1962, Open-File Report 62-137
Alfred R. Taylor
1962, Geologic Quadrangle 186
Richard Goldsmith
1962, Geologic Quadrangle 148
William Thordarson, M. S. Garber, G.E. Walker
1962, Open-File Report 62-134
D. W. Caldwell
1962, Open-File Report 62-24
Richard Goldsmith
1962, Geologic Quadrangle 176
G.C. Prescott Jr., J.A. Drake
1962, Open-File Report 62-105
Peter Popenoe, R. W. Bromery, J.R. Kirby
1962, Geophysical Investigations Map 365
R.M. Sawyer
1962, Open-File Report 62-117
John Stewart Vhay
1962, Bulletin 1112-G
Edward A. Sammel, John A. Baker
1962, Ground-water Series 2
The lower Ipswich River basin is that part of the Ipswich River drainage basin below the Geological Survey stream-gaging station at South Middleton in northeastern Massachusetts (fig. 1). It includes about 110 square miles between the gaging station at South Middleton and the Atlantic Ocean. This report presents basic data collected...
Water Resources Division, U.S. Geological Survey
1962, Report
The surface-water records for the 1962 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
Richard A. Robie
1962, Trace Elements Investigations 816
In the ten years since the publication of the national Bureau of Standards comprehensive tables of thermochemical properties, by Rossini and other (1952), a very large body of modern calorimetric and equilibrium data has become available. Because of the complex interrelations among many thermochemical data and the necessity for internal...
B.J. Kallman
1962, Chemist-Analyst (51) 75-76
Carboxylic esters and lactones react with alkaline hydroxylamine to yield hydroxamates; these in acidic solution form colored iron(III) complexes. A photometric determination of such esters and lactones is thus permitted and has been extensively applied ( I-6). Hestrin ( 3) utilized this method for the microdetermination of acetylcholine and his...
Harold Meisler
1962, Geological Society of America Bulletin (73) 1071-1082
Summit elevations in the Lebanon Valley, part of the Great Valley, range from 440 to 720 feet above msl (mean sea level). This range cannot be accounted for adequately by the peneplain concept. Although accordant summits, the chief evidence for peneplains, occur over large areas, summits are not accordant between...
Warren Hamilton
1962, Geological Society of America Bulletin (73) 511-516
The massive Salmon River Mountains of interior Idaho are bounded on the west by a belt 30 miles wide of post-Miocene, west-tilted normal-fault blocks and west-dipping monoclines. The belt is coincident with the western border zone of the middle Cretaceous Idaho batholith, as it extends from the west edge of the massive...
John L. Sincock
1962, Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners (16) 217-221
No abstract available....
James R. Gill
1962, Bulletin of the Geological Society of America (73) 725-735
Landslide blocks of latest Oligocene or earliest Miocene age are preserved at several localities in northwestern South Dakota and southeastern Montana. These tilted blocks contain Late Cretaceous to late Oligocene rocks and are unconformably overlain by nearly horizontal strata of the Arikaree Formation of Miocene age. Undisturbed rocks of late...
L. C. Pakiser, M. F. Kane
1962, Geophysics (27) 334-342
A narrow gravity minimum anomaly of amplitude 30 mgals indicates that northern Owens Valley, California, a narrow fault-bounded trough or graben filled with Cenozoic clastic deposits to a depth of as much as 8,000 ft. Seismic-refraction measurements support this conclusion. Aeromagnetic and gravity measurements define a small, dense, and magnetic body...
H.P. Eugster, D. R. Wones
1962, Journal of Petrology (3) 82-125
Annite, KFe3AISi3O10(OH)2 a member of the iron biotites and the ferrous analogue of phlogopite, has been synthesized and its phase relations have been determined as functions of temperature, fugacity of oxygen (fo2), and total pressure (Ptotal≈PH2O+PH2). A method for controlling fo2at high total pressures is described, and data for the 'oxygen...