A.H. Tuttle, Thomas R. Newell
1943, Water Supply Paper 917
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Page 7182, results 179526 - 179550
Publication Extents
Not all publications have extents, not all extents are completely accurateJohn S. Loofbourow
1943, Open-File Report 45-45
Philip Burke King
1943, Bulletin 940-B
L. D. Clark
1943, Open-File Report 43-35
W. S. White
1943, Open-File Report 43-34
D. C. Cox, J. F. de Albear, H. E. Hawkes
1943, Open-File Report 43-40
D. M. Larrabee, I.S. Fisher
1943, Open-File Report 43-59
Alonzo W. Quinn
1943, Open-File Report 79-354
No abstract available. ...
Glenn Lane Parker
1943, Water Supply Paper 935
J.J. Page, J.J. Norton, V.C. Fryklund
1943, Open-File Report 43-76
Allen P. Agnew, Allen V. Heyl Jr.
1943, Open-File Report 43-11
Walter S. White
1943, Open-File Report 42-1
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...
H.S. Davis
1943, Journal of Parasitology (29) 385-386
No abstract available. ...
Charles E. Kellogg
1943, Wildlife Leaflet 247
No abstract available....
A.E. Bellamy
1943, Wildlife Leaflet 244
No abstract available....
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...
D. Irvin Rasmussen, Marvin D. Wilde
1943, Wildlife Leaflet 246
No abstract available....
Ralph B. Nestler
1943, Journal of Wildlife Management (7) 418-419
No abstract available. ...
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...
Walter B. Lang
1943, Science (98) 583-584
No abstract available....
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...
P.D. Trask
1943, Science (98) 501-505
No abstract available....