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Page 2711, results 67751 - 67775

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Artesian water in Somervell County, Texas
Albert George Fiedler
1934, Water Supply Paper 660
Somervell County is part of the Grand Prairie region of north-central Texas. An excellent supply of artesian water is available from the Trinity reservoir at no great depth. The first flowing well in Somervell County was drilled in 1880, and the first flowing well in Glen Rose, the county seat,...
Ground-water supplies and irrigation in San Pedro Valley, Arizona
Kirk Bryan, G. E. P. Smith, Gerald A. Waring
1934, Open-File Report 67-31
The San Pedro Valley in southeastern Arizona extends from the International Boundary northward about 120 miles to the junction of the San Pedro River with the Gila River.  The river basin also extends about 75 miles into Mexico.  The valley varies in width from 5 to 20 miles, being widest...
Relation of stream‐flow to ground‐water levels
L.L. Harrold
1934, Eos, Transactions, American Geophysical Union (15) 414-416
In recent years the Water Resources Branch of the United States Geological Surrey has given considerable attention to the relation of ground‐water to stream‐flow. One locality in which this relation is being studied is about 13 miles from Washington, near Colesvllle, Maryland, where a Kinnison float‐gage is being maintained in a well In connection with the operation of a...
A study of salt‐water encroachment in the Galveston Area, Texas
Samuel F. Turner, Margaret D. Foster
1934, Eos, Transactions, American Geophysical Union (15) 432-435
A survey of the ground‐water resources of the region in which Houston and Galveston are situated was started in December 1930 by the United States Geological Survey in cooperation with the Texas Board of Water Engineers. In connection with this survey a special study is being made of the geochemical relations of the ground‐waters of an area about 25 miles wide and 90 miles long, extending from Galveston northwestward through Houston. This study considers the influence...
Report of the committee on underground‐water, 1933–34
D. G. Thompson
1934, Eos, Transactions, American Geophysical Union (15) 312-316
The by‐laws adopted at the meeting of the Section of Hydrology in 1933 provided that the membership of research committees should be reconstituted every three years. There have, accordingly, been some changes in the membership of the Committee on Underground‐Water. Certain members have retired because of pressure of other duties or because they are no...
The transmission of pressure in artesian aquifers
R.M. Leggette, G.H. Taylor
1934, Eos, Transactions, American Geophysical Union (15) 409-413
The water in artesian aquifers is confined under pressure. Under ideal conditions in a perfectly rigid artesian reservoir a change of pressure in one part of the reservoir should produce a corresponding change of pressure in all other parts of the reservoir. Theoretically, the transmission of pressure should take place rapidly and without any movement of water other than the small amount resulting from the compressibility of water. However,...
Appendix A—permeability
O. E. Meinzer
1934, Eos, Transactions, American Geophysical Union (15) 316-317
In the paper entitled “The measurement of the permeability of porous media for homogeneous fluids” by R. D. Wyckoff and others [42] a unit of permeability is proposed which is based on centimeters, seconds, and atmospheres of pressure (76 centimeters of mercury).In 1923, when the Hydrologic Laboratory of the United...
Report of the committee on chemistry of natural waters, 1933–34
C. S. Howard
1934, Eos, Transactions, American Geophysical Union (15) 322-325
The personnel of this Committee during the past year, practically the same as during the previous year, has been as follows: C. S. Howard, Chairman—United States Geological Survey, Washington, D.C. L. C. Case—Gypsy Oil Company, Tulsa, Oklahoma. W. D. Collins—United States Geological Survey, Washington, D.C. H. F. Flynn—United States Engineer Office, 35...
Appendix C—A selected list of papers relating to ground‐water hydrology
A.N. Sayre
1934, Eos, Transactions, American Geophysical Union (15) 318-320
In the following list brief statements have been added to certain references to call attention to special phases of ground‐water problems which are not apparent from the titles. Abstracts of most of these papers have been or will be published in the Annotated Bibliography of Economic Geology. ...
Appendix B—Lake and ground‐water levels
O. E. Meinzer
1934, Eos, Transactions, American Geophysical Union (15) 317-318
An outstanding achievement of the Section of Hydrology has been the work of the Committee on Glaciers in assembling the existing records of the advance and retreat of the glaciers in the Western States and in Alaska, encouraging various agencies in making periodic observations, systematizing and standardizing the work, and...
The chemical disinfection of trout ponds
F. F. Fish
1933, Transactions of the American Fisheries Society (63) 158-163
The need for knowledge concerning the prevention and control of fish diseases has never been greater than it is in this present era of economy when two fish must be raised in the same water which once supported but one. Fish pathologists have contributed a great deal to our knowledge...
The bleaching clays
P. G. Nutting
1933, Circular 3
Groundwater is one of Utah 's most extensive and valuable natural resources. Because of its widespread occurrence in both wet and dry areas, groundwater has been, and is a major factor affecting economic growth and development of the State. In some areas, groundwater is used to supplement streamflow for irrigation,...