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Publication Extents

Not all publications have extents, not all extents are completely accurate
Magnitude and frequency of floods in the United States: Part 10. The Great Basin
E. Butler, J.K. Reid, V.K. Berwick
1966, Water Supply Paper 1684
The probable magnitude of floods of any recurrence interval between 1.1 and 50 years for any stream in the Great Basin can be determined by methods presented in this report.The Great Basin comprises nearly all of Nevada, western Utah, eastern California, and parts of Idaho, Oregon, and Wyoming. The physiography...
Hydrology of the Upper Capibaribe Basin, Pernambuco, Brazil - A reconnaissance in an Area of Crystalline Rocks
Luiz Goncalves Chada Filho, Mario Dias Pessoa, William C. Sinclair
1966, Water Supply Paper 1663-E
The upper Capibaribe basin is the western three-fourths, approximately, of the valley of the river that empties into the Atlantic Ocean at Recife, the capital of the State of Pernambuco, Brazil. It is the part of the drainage basin that is within the Drought Polygon of northeast Brazil, and it...
Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska
J. E. Case, D.F. Barnes, George Plafker, S. L. Robbins
1966, Professional Paper 543-C
Sedimentary and volcanic rocks of Mesozoic and early Tertiary age form a roughly arcuate pattern in and around Prince William Sound, the epicentral region of the Alaska earthquake of 1964. These rocks include the Valdez Group, a predominantly slate and graywacke sequence of Jurassic and Cretaceous age, and the Orca...
Lake Bonneville: Geology and hydrology of the Weber Delta district, including Ogden, Utah
John Henry Frederick Feth, D.A. Barker, L.G. Moore, Randy J. Brown, C.E. Veirs
1966, Professional Paper 518
A cooperative investigation to determine the geology of the Weber Delta district, with emphasis on the occurrence and chemical quality of ground water, was made by the U.S. Geological Survey and the U.S. Bureau of Reclamation with the later assistance of the Utah State Engineer in the final preparation of...
Water and the Everglades
William J. Schneider
1966, Natural History (75) 32-41
This fundamental element, whether profuse or scarce, rules the life and character of Florida's great park. But water, like living space, is a resource that civilization demands in ever increasing quantities. Examined here are the economics of water use by Florida's east coast cities and its effects on Everglades ecology....
Magnetic data on the structure of the central Arctic Region
E. R. King, I. Zietz, L.R. Alldredge
1966, Geological Society of America Bulletin (77) 619-646
A study of 23,000 miles of total intensity aeromagnetic profiles in the central Arctic has been made by the U. S. Geological Survey and the U. S. Coast and Geodetic Survey. The profiles were flown at 20,000 feet above sea level and cover approximately 1,350,000 square miles of the Arctic Ocean between the North Pole...
Isotopic study of galenas from the upper Mississippi Valley, the Illinois-Kentucky, and some Appalachian Valley mineral districts
A. V. Heyl, M.H. Delevaux, R. E. Zartman, M. R. Brock
1966, Economic Geology (61) 933-961
Analyses of lead isotopes in galena in carbonate rock ore deposits collected from several mineralized districts in the Central and Eastern Interior of the United States support previous studies in establishing that the galena is anomalously radiogenic ("J"type")- This study, using care-fully selected samples to test some géologie relationships, shows region-wide and distrietwide systematic variations in isotope...
Virus diseases of salmonidae in the western United States. II. Aspects of pathogenesis
W. T. Yasutake, T. J. Parisot, G.W. Klontz
1965, Annals of the New York Academy of Sciences (126) 520-530
During the 10 to 15 years investigators from Europe and eastern United States have reported fish diseases of virus etiology. Rucker et al. in 1953 were the first to report a disease of possible virus origin in fish in the western United States. Since then many workers in the western...
Ground water in the alluvium of Otter Creek Basin, Oklahoma
Jerrald R. Hollowell
1965, Bulletin 27
Otter Creek basin comprises 287 square miles in Kiowa, Comanche, and Tillman Counties. The basin is not typical of southwestern Oklahoma in that it includes massive mountains and scattered knobs and peaks of the Wichita Mountains. Alluvium covers much of the southern half of the basin but is restricted to...
Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota
R. D. Cotter, H. L. Young, L. R. Petri, C. H. Prior
1965, Water Supply Paper 1759-C
Additional supplies of water are available near the municipalities or the west-central Mesabi Iron Range. The largest sources are the ground-water aquifers in the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift that probably have good water potential have been outlined. Surface-water supplies are negligible in the...
Summary of floods in the United States during 1960
J.O. Rostvedt
1965, Water Supply Paper 1790-B
This report describes the most outstanding floods in the United States during 1960. No major floods occurred during the year, although two floods caused severe damage the first in March and April in eastern Nebraska and adjacent areas, and the second in September in Puerto Rico.Unseasonal rains in mid-March caused...