W.G. Klontz
1968, American Fishes and U.S. Trout News (13) 21-22
Abstract not available...
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Page 5785, results 144601 - 144625
Publication Extents
Not all publications have extents, not all extents are completely accurateGary Wedemeyer
1968, Applied Microbiology (16) 661-662
Although dieldrin (1,2,3,4,10,10-hexachloro- 6,7-epoxy-1 ,4 ,4a ,5 ,6 ,7 ,8, 8a-octahydro-1 ,4-endo, exo-5, 8-dimethanonaphthalene) metabolism by mammals (F. Korte and H. Arent, Life Sci. 4:2017, 1965) and insects (D. F. Heath and M. Vanderkar, Brit. J. Ind. Med. 21:269, 1964) has been reported, little is known about the degradation of...
Arthur Maine Piper
1968, Trace Elements Investigations 873
No abstract available....
Orville B. Lloyd Jr., Hugh B. Wilder
1968, Report of Investigations of the North Carolina Department of Water and Air Resources, Division of Ground Water 5
In 1957, the National Park Service requested that the U. S. Geological Survey determine the quality and quantity of available ground water at selected sites within the Cape Hatteras National Seashore Recreational Area. A series of reports, Ground-Water Supply of Cape Hatteras National Seashore Recreational Area" by P. M. Brown...
I.H. Kantrowitz
1968, New York State Department of Environmental Conservation Report of Investigations RI-2
The Crown Point Fish Hatchery, one of several hatcheries operated by the New York State Conservation Department, is located in Crown Point Center, Essex County, on the eastern edge of the Adirondack Highlands and about 2 miles west of lake Champlain. Figure 1 is a location map of the vicinity...
Albert M. La Sala
1968, Connecticut Water Resources Bulletin 14
M. F. Kane, R. W. Bromery
E-an Zen, editor(s)
1968, Book chapter, Studies of Appalachian geology: Northern and maritime
No abstract available....
Henry W. Anderson Jr., A. S. Van Denburgh
1968, Water Supply Bulletin 25-2
The population of Island County has grown from 6,700 in 1940 to about 22,000 in 1964, causing a corresponding increase in the demand for water. Ground water is the only significant source of water within the county. Average annual precipitation ranges from less than 20 to more than 40 inches,...
Robert L. Klausing
1968, Bulletin 47
Cass County comprises an area of 1,749 square miles in the southeastern corner of North Dakota. About one-fourth of the county is in the Drift Prairie physiographic province; the rest is in the Red River Valley (Lake Agassiz basin) physiographic division....
John P. Bluemle, Henry Trapp Jr.
1968, Bulletin 44
Eddy and Foster Counties are in east-central North Dakota, high on the eastern flank of the Williston Basin. They are underlain by 3200 to 4300 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The uppermost formation, the Cretaceous Pierre Shale, lies directly beneath the glacial drift...
1968, Water Data Report CA-67-2
Water-resources investigations of the U.S. Geollogical Survey include the collection of water-quality data on the chemical and physical characteristics of surface-and ground-water supplies of the Nation. These data for the 1967 water year for the quality of surface waters in California are presented in this report. Data for a few...
1968, Water Data Report CA-67-1-2
The surface-water records for the 1967 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of...
1968, Water Data Report CA-67-1-1
The surface-water records for the 1967 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of...
Michael A. Cervione, I.G. Grossman, Chester E. Thomas Jr.
1968, Connecticut Water Resources Bulletin 16
This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the lower Thames and southeastern coastal river basins in cooperation with the Connecticut Water Resources Commission. The report area occupies about 440 square miles in the southeastern part of the...
Chester E. Thomas Jr., Michael A. Cervione Jr., I.G. Grossman
1968, Connecticut Water Resources Bulletin 15
The lower Thames and southeastern coastal river basins have a relatively abundant supply of water of generally good quality which is derived from streams entering the area and precipitation that has fallen on the area. Annual precipitation has ranged from about 32 inches to 65 inches and has averaged about...
K. Wolf
1968, Transactions of the American Fisheries Society (97) 510-510
This "book" is a collection of 31 carefully edited reports which are based upon presentations of highly qualified persons who were, for the most part, participants in a 3-day symposium held in 1965 and sponsored by the research branch of what is now the Federal Water Pollution Control Administration (FWPCA)....
Henry C. Barksdale
1968, Report
The water supply drought in the Northeast began in the autumn of 1961 and marked the beginning of a severe water shortage that continued with little relief through the summer of 1966. During this time, throughout much of the Northeast, water supplies remained below normal....
Water Resources Division, U.S. Geological Survey
1968, Water Data Report NM-67-1
The surface-water records for the 1967 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by...
A.M. La Sala Jr.
1968, Basin Planning Report ENB-3
The Erie-Niagara basin, New York, borders Lake Erie and the Niagara River and includes the principal part of their drainage basin in New York. The area extends from the Cattaraugus Creek basin on the south to the Tonawanda Creek basin on the north. The northern part of the area and...
W. E. Harding, B.K. Gilbert
1968, Basin Planning Report ENB-2
The Erie-Niagara basin contains about 2,000 square miles in western New York State. The drainage systems of the area discharge into Lake Erie and the Niagara River at an average rate of about 1,730 mgd (million gallons per day). Annual precipitation ranges from about 32 to 44 inches. Evapo-transpiration losses...
R.J. Archer, La Sala Jr., J.C. Kammerer
1968, Basin Planning Report ENB-4
The streams in the 2,000-square-mile Erie-Niagara basin of western New York contain mainly a calcium bicarbonate type of water whose dissolved-solids content generally varies between 140 and 240 ppm (parts per mill ion). Water "hardness" (expressed as CaCO3 ) is usually between 100 and 200 ppm, sulfate concentrations are between...
O. P. Hunt, R.M. Beall
1968, New York State Department of Environmental Conservation Report of Investigations RI-1
No abstract available....
R.J. Archer, La Sala Jr.
1968, Basin Planning Report ENB-5
This reconnaissance study of erosion and deposition of sediment in the Erie-Niagara basin indicates that the highest sediment yields, on the order of 1,000 tons per square mile per year, occur in streams that drain upland areas. In contrast, for example, from the lowland part of the Tonawanda Creek basin,...
D.F. Amend, J. L. Fryer
1968, Progressive Fish-Culturist (30) 168-172
The artificial propagation of salmon starts with the capture of adults as they ascend rivers to spawn. After capture, they are retained in specially constructed holding areas until sexually mature. Though holding periods vary with species, the spring chinook (Oncorhynchus tshawytsca) may be held as long as 4 months before...
G. W. Walker, D. A. Swanson
1968, Bulletin Volcanologique (32) 579-585
[No abstract available]...