G.E. Goodspeed, P.J. Fitzsimmons
1943, Open-File Report 46-27
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Page 6447, results 161151 - 161175
Publication Extents
Not all publications have extents, not all extents are completely accurateM. R. Klepper
1943, Open-File Report 46-7
Charles Brian Read, R.D. Sample, H.H. Sullwold Jr.
1943, Open-File Report 43-24
Walter S. White
1943, Open-File Report 42-1
Allen P. Agnew, Allen V. Heyl Jr.
1943, Open-File Report 43-11
Eugene Callaghan, C.J. Vitaliano, S.E. Clabaugh, S. Warren Hobbs
1943, Open-File Report 43-12
Nels P. Peterson, S.C. Creasey
1943, Open-File Report 43-14
J. B. Hadley, H.H. Sullwold Jr.
1943, Open-File Report 44-8
Paul Averitt, G. Donald Eberlein, Edwin Butt Eckel
1943, Open-File Report 43-84
A. B. Griggs, F. G. Wells, E.L. Stephenson
1943, Open-File Report 43-22
F. C. Calkins, B. S. Butler, V. C. Heikes
1943, Professional Paper 201
The first systematic geological study of the Wasatch Range was done by the Fortieth Parallel Survey,1 mainly by Clarence King and S. F. Emmons. These pioneers broadly outlined the stratigraphy and distribution of the rocks and. prepared regional geologic maps that for parts of the region have not yet been...
David White
C.B. Read, editor(s)
1943, Professional Paper 197-C
D. C. Cox, J. F. de Albear, H. E. Hawkes
1943, Open-File Report 43-40
Walter S. White, John H. Eric, Thomas William Amsden
1943, Open-File Report 79-352
No abstract available....
J.F. Smith Jr. , L.L. Ray
1943, Geological Society of America Bulletin (54) 891-924
In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of...
Hugh Dinsmore Miser
1943, Economic Geology (38) 91-118
An important chapter of the total geologic history of the Ouachita Mountains is revealed by the quartz veins and crystals. These and the associated minerals are hydrothermal deposits of probable magmatic origin, formed during the closing stage of the mid-Permsylvanian orogeny. The metalliferous deposits of the Ouachita Mountains appear to...
Lyman C. Huff
1943, Eos, Transactions, American Geophysical Union (24) 573-580
Water‐levels in wells, which are utilized by the hydrologist as a measure of ground‐water storage, customarily are measured in terms of distance below a convenient measuring point and expressed with reference to a fixed datum. Datum‐planes or surfaces of several types have been used—each serving some particular purpose advantageously. These...
C. E. Jacob
1943, Eos, Transactions, American Geophysical Union (24) 564-573
Long Island simulates in a general way an aquifer in the form of an infinite strip confined between parallel boundaries at constant head (sea‐level), over which recharge precipitation is assumedly uniform. The non‐steady flow of water in this idealized system is analyzed assuming provisionally that the effective thickness of saturated...
John T. Hack
1943, American Antiquity (8) 235-241
This report is based on two months reconnaissance in the summer of 1941 in the Eden Valley, Wyoming. The work is as yet far from complete and the conclusions presented here must be regarded as tentative. It is hoped that in the future more extensive geological work may be undertaken.The...
Walter B. Lang
1943, Science (98) 173-174
No abstract available....
Leland K. Wenzel, A.L. Greenlee
1943, Eos, Transactions, American Geophysical Union (24) 547-564
Ground‐water has long been recognized as one of our important natural resources, but only in about the last 20 years has concentrated effort been made to place ground‐water hydrology on a quantitative basis. The quantitative approach to ground‐water work has been brought about largely through the leadership of O. E....
Jewell J. Glass
1943, Eos, Transactions, American Geophysical Union (24) 252-257
The recent discovery of the widespread occurrence of helvite, a beryllium‐bearing mineral, at Iron Mountain, New Mexico, has aroused interest in the commercial possibilities of a mineral which heretofore has been considered to have only scientific significance. Helvite contains about 13 per cent beryllium oxide as compared with five to...
W. G. Hoyt, Bertram Barnes, H.B.S. Cooke, E.S. Cullings, G.A. Hathaway, Karl R. Jetter, N.H. Leupold, Phillip Light, C. C. McDonald, F.T. Mavis, L.K. Sherman, Waldo E. Smith, F. Snyder, H.G. Wilm
1943, Eos, Transactions, American Geophysical Union (24) 422-423
The Committee on Runoff was not formally constituted until February 6, 1943, when the members of the Section, as listed above, were asked to serve. At the suggestion of President CHURCH the Committee has been so selected that there is Nation‐wide geographic distribution from West to East with the majority...
O. E. Meinzer
1943, Article
The very large service which the geologists and engineers trained in ground‐water hydrology are rendering in this country in the prosecution of the war is due largely to the effective organization for this purpose. The Federal agency in which this service centers is the Water Resources Branch of the United...
Francois E. Matthes
1943, Eos, Transactions, American Geophysical Union (244) 389-401
The personnel of the Committee at present is as follows:Harry Fielding Reid, Professor Emeritus of Geology, Johns Hopkins University, 608 Cathedral Street, Baltimore, MarylandWilliam H. Hobbs, Professor Emeritus of Geology, University of Michigan, Ann Arbor, Michigan Colonel Lawrence Martin, Chief, Division of Maps, Library of Congress, Washington, D.C.James E. Church,...