Annotated bibliography of the analytical chemistry of niobium and tantalum, January 1935-June 1953
Frank Cuttitta
1957, Bulletin 1029-A
Some pegmatite deposits in southeastern Alaska
C.L. Sainsbury
1957, Bulletin 1024-G
Bikini and nearby atolls, Marshall Islands; seismic-refraction studies of Eniwetok Atoll
R.W. Raitt
1957, Professional Paper 260-S
The deep channel and alluvial deposits of the Ohio Valley in Kentucky
Eugene H. Walker
1957, Water Supply Paper 1411
The alluvial deposits of Pleistocene age in the Ohio Valley form a ground-water reservoir of large storage capacity and yield. In this region it is the only source of large supplies of water that are both cool and of good quality the year round. The reservoir is heavily drawn upon,...
Geology and ground water, Heart Mountain and Chapman Bench Divisions, Shoshone irrigation project, Wyoming
Frank Albert Swenson, Herbert Swenson
1957, Water Supply Paper 1418
No abstract available....
Preliminary geologic map of the west-central part of the Minnekahta quadrangle, Fall River County, South Dakota
V.R. Wilmarth, R.D. Smith
1957, Miscellaneous Field Studies Map 67
No abstract available....
Preliminary geologic map of the southwest part of the Minnekahta quadrangle, Fall River County, South Dakota
V.R. Wilmarth, R.D. Smith
1957, Miscellaneous Field Studies Map 70
No abstract available....
Preliminary geologic map of the east-central part of the Minnekahta quadrangle, Fall River County, South Dakota
V.R. Wilmarth, R.D. Smith
1957, Miscellaneous Field Studies Map 68
No abstract available....
Mineral deposits of Central America, with a section on manganese deposits of Panama
Ralph Jackson Roberts, Earl Montgomery Irving, F. S. Simons
1957, Bulletin 1034
The mineral deposits of Central America were studied between 1942 and 1945, in cooperation with the United States Department of State and the Foreign Economic Administration. Emphasis was originally placed on the study of strategic-mineral deposits, especially of antimony, chromite, manganese, quartz, and mica, but deposits of other minerals that...
Preliminary geologic map and sections of the magnesite belt, Stevens County, Washington
Ian Campbell, J.S. Loofbourow
1957, Miscellaneous Field Studies Map 117
No abstract available....
Geology and ground-water resources of the Lower Marias Irrigation Project, Montana
Frank Albert Swenson
1957, Water Supply Paper 1460-B
Hawaiian volcanoes during 1954
Gordon Andrew Macdonald, Jerry P. Eaton
1957, Bulletin 1061-B
Geology and ground-water resources of the lower Lodgepole Creek drainage basin, Nebraska, with a section on chemical quality of the water
Louis Jay Bjorklund, Eugene R. Jochens
1957, Water Supply Paper 1410
The area described is almost wholly in Nebraska and is the drainage basin of Lodgepole Creek from the Wyoming State line to the Colorado State line, a distance along the stream valley of about 95 miles. It covers about 1,950 square miles. The purposes of the study were to ascertain...
Water resources summary for southern California, 1956
Walter Hofmann, W. C. Peterson
1957, Circular 399
Surface water supply of the United States, 1955, Part IX, Colorado River basin
Water Resources Division, U.S. Geological Survey
1957, Water Supply Paper 1393
Geology of the Precambrian rocks of the Keystone pegmatite district, southern Black Hills, South Dakota
James Jennings Norton
1957, Open-File Report 57-84
Geology of Gabbs and vicinity, Nye County, Nevada
Charles J. Vitaliano, Eugene Callaghan, Norman J. Silberling
1957, Miscellaneous Field Studies Map 52
The geologic map of Gabbs and vicinity covers approximately 105 square miles of the northwestern part of the Paradise Peak quadrangle. The present report stresses the igneous, metamorphic, and structural geology. The map published at this time shows, (1) the distribution of igneous rocks in the area, (2) the relationship...
Surface water supply of the United States, 1955, Part XII, Pacific slope basins in Washington and upper Columbia River basin
Water Resources Division, U.S. Geological Survey
1957, Water Supply Paper 1396
Glacial features and surficial deposits of the Malaspina district, Alaska
George Plafker, Don John Miller
1957, Open-File Report 57-91
The Malaspina district extends about 50 miles along the north shore of the Gulf of Alaska from Icy Bay and the Guyot Glacier on the west to Yakutat Bay and Disenchantment Bay on the east (see index map). The district includes a coastal lowland flanked on the north by a...
Surface water supply of eastern and central North Carolina
Edward B. Rice
1957, Open-File Report 57-96
None of the many factors that influence the economic growth of eastern and central North Carolina plays a more important role than water. Adequate water supply for municipal, rural domestic, industrial, and agricultural uses, is a basic need of any region....
Geologic investigations of radioactive deposits, semiannual progress report, December 1, 1956 to May 31, 1957
Water Resources Division, U.S. Geological Survey
1957, Trace Elements Investigations 690
No abstract available....
Notom 4 NW quadrangle, Utah
J. F. Smith Jr., L.C. Huff, E. N. Hinrichs, R. G. Luedke
1957, Miscellaneous Field Studies Map 113
Agathla Peak NW quadrangle, Arizona-Utah
I. J. Witkind
1957, Miscellaneous Field Studies Map 88
A field method for the determination of calcium and magnesium in limestone and dolomite
Leonard Shapiro, Walter Wallace Brannock
1957, Open-File Report 57-99
The method is an adaptation of a procedure described by Betz and Noll1 in 1950. Calcium and magnesium are determined by visual titration using Versene (disodium ethylenediamine tetraacetate) with Murexide (ammonium purpurate) as the indicator for calcium and Eriochrome Black T as the indicator for magnesium....
Drainage area data for Alabama streams
J.S. Stallings, L.B. Peirce
1957, Open-File Report 57-106
The drainage area of a river basin is an important parameter in many engineering equations used for hydrologic design. It is not a parameter, however, that always requires precise measurement. Factors in the hydrologic cycle such as rainfall, runoff, transpiration, and infiltration cannot be measured nearly as closely as drainage...