Water Resources Division, U.S. Geological Survey
1944, Water Supply Paper 974
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1944, Water Supply Paper 956
Water Resources Division, U.S. Geological Survey
1944, Water Supply Paper 951
Water Resources Division, U.S. Geological Survey
1944, Water Supply Paper 954
Water Resources Division, U.S. Geological Survey
1944, Water Supply Paper 955
Allen F. Agnew, Allen V. Heyl
1944, Open-File Report 44-24
J.S. Cullison, A.E. Weissenborn
1944, Open-File Report 44-23
J.C. Miller
1944, Open-File Report 44-10
No abstract available....
Archibald L. Slaughter, Stephen Edmund Clabaugh
1944, Trace Elements Investigations 3
W. D. Collins, S. K. Love
1944, Water Supply Paper 950
F.G. Ashbrook
1944, Wildlife Leaflet 262
1944, Wildlife Leaflet 263
H.J. Spencer
1944, Wildlife Leaflet 264
E. W. Surber
1944, Transactions of the American Fisheries Society (74) 338-349
Ammonia, nitrite, nitrate, and organic nitrogen were determined at 10‐day intervals for 24 ponds at Leetown, West Virginia. These ponds were stocked with 15,000 smallmouth black bass fry per acre and all fish reared in them were counted individually and weighed when the ponds were drained after an average...
Lawrence C. Crawford
1944, Water Supply Bulletin 2
The State and Federal cooperative program for the systematic collection of stream-flow records in Iowa was initiated in L914, although a few records were obtained by special arrangements during an earlier period. Since the beginning of the cooperative program measurements of stage or discharge have been obtained at about 100...
C. E. Jacob
1944, Eos, Transactions, American Geophysical Union (25) 928-939
A brief though concise statement of the history of ground‐water studies on Long Island, beginning with the early water‐level observations in Brooklyn by STODDARD in 1854, was given by THOMPSON [see 7 of “References” at end of paper]. These and other early data were considered later by LEGGETTE [8]. He...
Geological Division Kentucky
1944, Report
No abstract available....
George Clayton Kennedy
1944, Economic Geology (39) 25-36
The solubility of silica glass in water has been determined through the temperature range 200 degrees C. to 420 degrees C. at a pressure of 300 atmospheres. Some previous investigations of solubility of silica in water, it is believed, have indicated a too great solubility as a result of failure...
A. M. Piper
1944, Eos, Transactions, American Geophysical Union (25) 914-928
This paper outlines certain fundamental principles in a graphic procedure which appears to be an effective tool in segregating analytical data for critical study with respect to sources of the dissolved constituents in waters, modifications in the character of a water as it passes through an area, and related geochemical...
P.D. Trask
1944, Eos, Transactions, American Geophysical Union (25) 617-618
Owing to the good fortune of being stationed near the new volcano Parícutin when it first erupted, I was able to visit it when it was only a week old. As my observations have been recorded in full in a previous article [see 1 of “References” at end of paper],...
D. E. White
1944, Eos, Transactions, American Geophysical Union (25) 621-628
Parícutin's volcanic activity during its first year of life included a number of periods characterized by flowing lava. The length of time of individual periods ranged from a few days up to more than a month, and were separated by intervals during which little or no lava flowed at the...
Charles Milton
1944, Eos, Transactions, American Geophysical Union (25) 618-621
The small collection of lava‐flows, bombs, and ashes from Parícutin, which are to be briefly described, was obtained from several sources and is far from being as completely representative of the volcanic history of the region as one might wish. Until, however, an adequate study is made, these specimens may...
Robert E. Fellows
1944, Eos, Transactions, American Geophysical Union (25) 653-659
The most important factor which would reduce confusion in fabric analyses is the expanded use of partial diagrams. The purpose of this paper is to stress the significance of partial diagrams in a consideration of some confusing aspects of petrofabrics.Any statistical study results in the accumulation of a mass of...
S. W. Lohman, H.F. Blaney, J. Harlan Bretz, Edward Burwell Jr., V.C. Fishel, Willard Gardner, C. S. Howard, G.W. Musgrave, A. M. Piper, N.A. Rose, A.N. Sayre, H.T. Stearns, V. T. Stringfield
1944, Eos, Transactions, American Geophysical Union (25) 712-721
The Chairman extends an apology to G. W. MUSGRAVE for omission of his name from the list of members given in the report of the Committee on Ground Water for 1942–43.The response from members of the Committee in general has been very gratifying and is much appreciated. Four new members,...
A.N. Sayre
1944, Eos, Transactions, American Geophysical Union (25) 724-725
In June, 1943, the United States Geological Survey assigned two ground‐water geologists, A. N. SAYRE and G. C. TAYLOR, Jr., to study water‐supply problems in Central America for the Coordinator of Inter‐American Affairs and to make recommendations for remedial measures to provide water for cities and towns, especially along the...