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Publication Extents

Not all publications have extents, not all extents are completely accurate
Index of surface-water records, part 7, Lower Mississippi River basin, to September 30, 1950
Water Resources Division, U.S. Geological Survey
1951, Circular 144
The index lists the steam-flow and reservoir stations in the Lower Mississippi River Basin for which records have been or are to be published for periods prior to September 30, 1950. The stations are listed in downstream order. Tributary streams are indicated by indention. Station names are given in their...
Flood of August 1-6, 1950, at Wichita Falls, Texas
Ivan Dale Yost
1951, Circular 99
Floods occurred on streams in the vicinity of Wichita Falls, Tex., during the period Aug. 1-6, 1950, as a result of heavy rains falling immediately southwest of the city on August 1, 1950. Serious flooding occurred along Holliday Creek in the city, necessitating the evacuation of about five hundred families...
Index of surface-water records, part 4, St. Lawrence River Basin, to September 30, 1950
Water Resources Division, U.S. Geological Survey
1951, Circular 123
The index lists the stream-flow and reservoir stations in the St. Lawrence River Basin for which records have been or are to be published for periods prior to September 30, 1950. The stations are listed in downstream order. Tributary streams are indicated by indention. Station names are given in their...
Progress report, chemical quality of the surface waters in the Loup River basin, Nebraska
John G. Connor
1951, Circular 107
The Loup River and its tributaries transport moderate amounts of siliceous minerals from the sand hills region of north-central Nebraska to the Platte River near Columbus, Nebr. Predominant chemical characteristics of these waters are a high percentage of silica, moderate hardness, and a low percentage of sodium. The composition of...
Selected abstracts on engineering geology and related subjects
Severine Hansenne Britt
1951, Circular 75
Interlayered sand, silt, and clay of middle Eocene to late Paleocene age in east-central Georgia form the Gordon aquifer system which ranges in thickness from about 20 to 180 ft. Estimated transmissivities range from 620 to 13,000 sq ft/day. During 1980, approximately 24 million gpd (gallons per day) was withdrawn...
Bibliography of U.S. Geological Survey publications relating to coal, 1882-1949
Louise R. Berryhill
1951, Circular 86
All publications of the U. S. Geological Survey relating to coal published prior to January 1, 1950, are listed in the following Bibliography and in an Index beginning on page 18. The Bibliography gives complete titles of reports, listed numerically under several series headings as follows: Annual Reports, Monographs, Professional...
Coking-coal deposits of the western United States
Louise R. Berryhill, Paul Averitt
1951, Circular 90
Geohydrologic systems in the Anadarko basin in the central United States are controlled by topography, climate, geologic structures, and aquifer hydraulic properties, all of which are the result of past geologic and hydrologic processes, including tectonics and diagenesis. From Late Cambrian through Middle Ordovician time, a generally transgressive but cyclic...
Ground-water conditions in the Dutch Flats area, Scotts Bluff and Sioux Counties, Nebraska, with a section on chemical quality of the ground water
H. M. Babcock, F. N. Visher, W. H. Durum
1951, Circular 126
The U.S. Department of the Interior (DOI) studied contamination induced by irrigation drainage in 26 areas of the Western United States during 1986-95. Comprehensive compilation, synthesis, and evaluation of the data resulting from these studies were initiated by DOI in 1992. Soils and ground water in irrigated areas of the...
Ground-water resources of Baker Valley, Baker County, Oregon
F.D. Trauger
1951, Open-File Report 51-155
The Baker Valley is the southern part of a small oval-shaped inter-montane structural basin located near tie southeastern edge of the Blue Mountains of northeastern Oregon. The Powder River enters and leaves the valley through narrow rock gorges. The alluviated basin floor at an altitude of about 3,400 feet is...
Discussion of “a comparison of several heat and mass transfer networks of interest in water conservation”
Ernest R. Anderson, J. J. Marciano, G. E. Harbeck Jr., H. F. Poppendiek, M. Tribus
1951, Eos, Transactions, American Geophysical Union (32) 931-932
The use of electrical networks to describe heat‐ and mass‐transfer problems is an interesting concept and undoubtedly will be of considerable value in future water‐loss investigations, provided the processes involved can be represented, electrically, with sufficient accuracy.Although it is true that errors in measurement of water‐surface temperature may arise when...
Geologic history of sea water: An attempt to state the problem
William W. Rubey
1951, Geological Society of America Bulletin (62) 1111-1148
Paleontology and biochemistry together may yield fairly definite information, eventually, about the paleochemistry of sea water and atmosphere. Several less conclusive lines of evidence now available suggest that the composition of both sea water and atmosphere may have varied somewhat during the past; but the geologic record indicates that these...
Report of the Committee on Ground Water, 1949–1950
S.W. Lohman
1951, Eos, Transactions, American Geophysical Union (32) 769-772
The present report concludes the duties of the above Committee, and the Chairman takes this opportunity to thank the members and others for their splendid cooperation during the triennium ended June 30, 1950. Another in the series of reports on hydrology and physiography of limestone terranes, by A. C. Swinnerton, is given as...