John C. Reed
1939, Bulletin 897-D
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1939, Water Supply Paper 854
Water Resources Division, U.S. Geological Survey
1939, Water Supply Paper 864
R.O. Helland
1939, Open-File Report 39-8
L.G. Henbest, K. E. Lohman, W. C. Mansfield
1939, Professional Paper 189-G
David A. Andrews
1939, Bulletin 906-B
Charles Edgar Erdmann
1939, Open-File Report 39-1
C.F. Bassett
1939, Wildlife Leaflet 128
Division Of Wildlife Research
1939, Wildlife Leaflet 140
C.K. Wentworth, L.L. Ray
1939, Geological Society of America Bulletin (47) 879-934
No abstract available....
F.M. Uhler, Stephen Creech
1939, Wildlife Leaflet 149
No abstract available....
Frank G. Grimes
1939, Wildlife Leaflet 147
No abstract available....
U.S. Division Of Wildlife Refuges
1939, Wildlife Leaflet 146
No abstract available....
Frederick Charles Lincoln
1939, Wildlife Leaflet 145
No abstract available....
C. E. Jacob
1939, Eos, Transactions, American Geophysical Union (20) 666-674
Perhaps one of the chief interests of ground‐water hydrologists is the study of water‐level fluctuations. Since the beginning of the science of hydrology attempts have been made to interpret these phenomena and determine their significance. On the basis of actual observations and “with special reference to Long Island, New York,”...
F. Snyder
1939, Eos, Transactions, American Geophysical Union (20) 725-738
The problem of transforming observed precipitation into stream‐flow for a natural drainage‐basin can be divided into two parts. The first part requires a procedure for determining the amount and kind of runoff that occurs under various conditions. The second part is concerned with the shaping of the runoff into a...
T. W. Robinson
1939, Eos, Transactions, American Geophysical Union 656-665
It is quite generally known that ocean‐tides produce fluctuations of the water‐level in wells of the artesian type located close to the seashore by periodically changing the external load on the aquifer [see 1 of “References” at end of paper]. Fluctuations of ground‐water as a result of earth‐tides, however, are...
E.B. Eckel
1939, Science (89) 37-38
No abstract available....
P. G. Nutting
1939, Science (89) 131-131
No abstract available....
J.S. Vhay
1939, Eos, Transactions, American Geophysical Union (20) 433-437
The Livingston Formation is a series of pyroclastic rocks several thousand feet thick cropping out on the north side of the Beartooth Mountains. These pyroclastic rocks grade laterally into the Claggett, Judith River, Bearpaw, and Lennep formations of the Montana Group, according to Stone and Calvert [see 1 of references...
Irwin Roman
1939, Eos, Transactions, American Geophysical Union (20) 298-303
In addition to projects such as those reported in parts I and II above, the Section of Geophysics of the Federal Government has undertaken a considerable amount of fundamental research.Two such field‐projects may be mentioned, one a magnetometric study in the Comstock District of Nevada, and the other a resistivity‐study...
R.M. Wilson
1939, Eos, Transactions, American Geophysical Union (20) 306-308
Those of you who attended the annual meeting of this Section on April 27, 1938, heard a paper entitled “A method for introducing a new standard of length” that was presented by Professor Philip Klssara, calling attention to the Bill then in Congress proposing to redefine the length of the...
O. E. Meinzer
1939, Eos, Transactions, American Geophysical Union (20) 674-677
The hydrologists who are concerned with the study of the water that occurs below the land‐surface feel strongly the need of better agreement among the different countries as to the fundamental concepts of this branch of hydrology and as to technical terms to designate these concepts. For this reason, the...
F.W. Lee
1939, Eos, Transactions, American Geophysical Union (20) 383-389
Early application of electricity to the ground was of interest particularly to telegraphy especially when it was first commercially applied. There was available at that time the Newtonian analysis of sources and sinks in a semi‐infinite medium which could be applied directly to ground‐contacts. Experiments conducted at that time showed...
Eugene Callaghan
1939, Eos, Transactions, American Geophysical Union (20) 438-452
As a consequence of the detailed investigation of the alunite and other mineral deposits of the Marysvale Region in southwest‐central Utah, opportunity was afforded to map and study the succession of volcanic rocks that underlie most of this area. The Marysvale Region is part of a large area of volcanic...