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Salinity of the lower Savannah River in relation to stream‐flow and tidal action
William L. Lamar
1940, Eos, Transactions, American Geophysical Union (21) 463-470
In order to obtain information needed in planning for industrial development along the Savannah River and in the city of Savannah, Georgia, a study of the salinity of the Savannah River was undertaken by the Geological Survey, United States Department of the Interior, in cooperation with the Georgia Division of...
Ground-water resources of Kansas
R.C. Moore, S. W. Lohman, J.C. Frye, H.A. Waite, Thad G. McLaughlin, Bruce Latta
1940, Kansas Geological Survey Bulletin (1940) 1-112
Introduction: Water is a necessity of life. Accordingly, every person is deeply interested in the subject of water supply. He knows that he must have water to drink. He depends indirectly on water for all his food and clothing. He may want water in which to wash. Civilized man has...
Supplementary report on the ground-water supplies of the Atlantic City region
Henry C. Barksdale, Raymond W. Sundstrom, Maurice S. Brunstein
1936, Special Report 6
This report is the second progress report on the ground-water investigations in the Atlantic City region. Many important problems still remain to be solved, however, and it is in no sense a final report. The report covers the area immediately surrounding Atlantic City, extending from Brigantine to Sea Isle City along...
Fluctuations of ground‐water levels in Utah
G.H. Taylor
1936, Eos, Transactions, American Geophysical Union (17) 378-382
Long‐time continuous records of the fluctuations of ground‐water levels have been obtained at relatively few locations in the United States. Among the few available records for Utah that extend continuously over a period of a year or more are those made in the Jordan River and Ogden valleys by the...
Long‐time records of ground‐water levels on Long Island, New York
R.M. Leggette
1936, Eos, Transactions, American Geophysical Union (17) 341-344
As early at 1851 the need for information as to the position of the water‐table was recognized by workers on Long Island. In that year water‐level measurements were made in about 32 domestic wells in the southern part of Kings and Queens counties, New York (W. J. McAlpine, Report made...
Deep‐well salinity‐exploration
A.G. Fiedler
1933, Eos, Transactions, American Geophysical Union (14) 478-480
One of the outstanding accomplishments of recent years in connection with the study of the geologic source of groundwater and the quality of water yielded by different formations has been the development of methods and equipment for the exploration of wells. The description and use of the deep‐well current‐meter on well‐exploration work in Hawaii and New...
Geology and ore deposits of the Pioche district, Nevada
L.G. Westgate, Adolph Knopf
1932, Professional Paper 171
LOCATION AND SURFACE FEATURES The Bristol Range, Highland, and Ely Range quadrangles make up the larger part of a. rectangular area 35 miles north and south by 24 miles east and west, which lies 19 miles west of the Nevada-Utah line and about 250 miles southwest of Salt Lake...
Underground water in the valleys of Utah Lake and Jordan River, Utah
George Burr Richardson
1906, Water Supply Paper 157
The valleys of Utah Lake and Jordan River are situated in north-central Utah, in the extreme eastern part of the Great Basin. The lofty Wasatch Range (Pl. I), the westernmost of the Rocky Mountain system, limits the valleys on the east, and relatively low basin ranges - the Oquirrh, Lake,...
Charleston folio, West Virginia
Marius R. Campbell
1901, Folios of the Geologic Atlas 72
The Charleston quadrangle embraces an area of 938 square miles, extending from latitude 38° on the south to 38°30' to the north, and from longitude 81° 30' on the east to 82° on the west.  The quadrangle is located in the State of West Virginia, including parts of the counties of Kanawha,...