Montis Ruhl Klepper, Water Resources Division, U.S. Geological Survey
1943, Open-File Report 43-91
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Page 6393, results 159801 - 159825
Publication Extents
Not all publications have extents, not all extents are completely accurateEugene Callaghan, D.M. Lemmon
1943, Bulletin 931-A
No abstract available....
Water Resources Division, U.S. Geological Survey
1943, Bulletin 930-D
Water Resources Division, U.S. Geological Survey
1943, Bulletin 930-C
Paul Averitt, G. Donald Eberlein, Edwin Butt Eckel
1943, Open-File Report 43-84
Charles Brian Read, R.D. Sample, H.H. Sullwold Jr.
1943, Open-File Report 43-24
M. R. Klepper
1943, Open-File Report 46-7
C.W. Chesterman, P. Joralemon, M. R. Klepper
1943, Open-File Report 46-17
G.E. Goodspeed, P.J. Fitzsimmons
1943, Open-File Report 46-27
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
J. B. Hadley, H.H. Sullwold Jr.
1943, Open-File Report 44-8
Nels P. Peterson, S.C. Creasey
1943, Open-File Report 43-14
H.R. Cornwell
1943, Open-File Report 45-9
M. R. Klepper
1943, Open-File Report 43-90
A. H. Koschmann
1943, Open-File Report 43-6
D. C. Cox, J. F. de Albear, H. E. Hawkes
1943, Open-File Report 43-40
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...
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...