Correlation of ground‐water levels and precipitation on Long Island, New York
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...
Gigantic drying cracks in Animas Valley, New Mexico
Walter B. Lang
1943, Science (98) 583-584
No abstract available....
The Finley Site: Antiquity of the Finley Site
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...
The Mexican volcano Paricutin
P.D. Trask
1943, Science (98) 501-505
No abstract available....
The mosses of Luray Cavern, Virginia
Walter B. Lang
1943, Science (98) 173-174
No abstract available....
A method for determining transmissibility‐ and storage‐coefficients by tests of multiple well‐systems
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....
Helvite, a product of magmatic emanations at Iron Mountain, Sierra Socorro Counties, New Mexico
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...
Report of Committee on Runoff, 1942–43
W. G. Hoyt, Bertram Barnes, H.L. Cook, 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...
Appendix B—The work of the Geological Survey and cooperating state agencies on ground water for war purposes
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...
Report of Committee on Glaciers, 1942–43
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,...
The nickel deposits of Yakobi Island, southeastern Alaska
George C. Kennedy
1943, Eos, Transactions, American Geophysical Union (24) 257-257
Some of the large, low‐grade nickel‐copper deposits of Bohemia Basin, Yakobi Island, south‐eastern Alaska, which previously had been mapped and studied by the United States Geological Survey, were explored during parts of 1941 and 1942 by the United States Bureau of Mines. The Gealogical Survey interpreted the geologic features of...
Appendix C—Report on research in the field of ground water being conducted by oil companies
N.A. Rose
1943, Eos, Transactions, American Geophysical Union (24) 420-421
In view of the shortness of time since the appointment of the writer to the Committee on Ground Water this report is confined to the technology and problems in the Gulf Coast Oil Province. Of course, many of the methods and practices would apply to most parts of the country...
Flowage and recrystallization in paleozoic quartzites
Robert E. Fellows
1943, Eos, Transactions, American Geophysical Union (24) 271-271
The lower limit of visible traces of penetrative movement in quartz‐rich rocks can be defined by studies of orientations and mutual relations of grains. Intensity of deformation in the central Appalachians decreases gradually from the crystalline Piedmont toward the north, northwest, and west perpendicular to the regional trend. The author...
Appendix A—The work of the International Commission on Subterranean Water in the Western Hemisphere
O. E. Meinzer
1943, Eos, Transactions, American Geophysical Union (24) 418-418
No abstract available. ...
The manganese oxide minerals, a preliminary report
Michael Fleischer, W.E. Richmond
1943, Economic Geology (38) 269-286
This paper summarizes the results obtained thus far in an intensive study of the manganese oxide minerals. X-ray powder photographs, supplemented by chemical tests, have proved to be the best means for identifying these minerals. Formulas are suggested. Physical properties and X-ray data are listed for the commoner minerals and...
Diarrhea in domestic rabbits
Edward L. Vail, Frank D. McKenney
1943, Wildlife Leaflet 245
No abstract available....
Preliminary report on water storage capacity of unconsolidated deposits beneath the Lompoc Plain, Santa Barbara County, California
Joseph E. Upson
1943, Report
The Lompoc Plain is the central lowland of a topographic and structural basin that forms the western and lower part of the Santa Ynes Valley in Santa Barbara County, California. It extends inland about 11 miles from the coast and is 1 mile fto about 3 miles wide....
Recipes for cooking domestic rabbit meat
U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 240
No abstract available....
Enteritis, or so-called bloat, in domestic rabbits
U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 239
No abstract available....
Structural determinations from diamond drilling
John Beaver Mertie
1943, Economic Geology (38) 298-312
Several problems may arise in the geometrical determinations of strike and dip from core drilling. If the stratigraphic or structural surfaces are plane, as the bedding planes of a homocline, two problems may exist, depending upon whether the drill cores do or do not penetrate to some recognizable horizon. The...
Rabbit-pen construction in relation to sore hocks
George S. Templeton
1943, Wildlife Leaflet 242
No abstract available....
Control of coccidiosis in rabbits
Edward L. Vail
1943, Wildlife Leaflet 241
No abstract available....
Klamath Basin National Wildlife Refuges, Oregon and California
Stanley G. Jewett
1943, Wildlife Leaflet 238
No abstract available....
Control of woodchucks
Branch of Predator and Rodent Control U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 237
No abstract available....
Protecting victory gardens from animal pests
Branch of Predator and Rodent Control U.S. Fish and Wildlife Service
1943, Wildlife Leaflet 236
No abstract available....
