U.S. Bureau of Sport Fisheries and Wildlife
1967, Resource Publication 42
No abstract available...
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Publication Extents
Not all publications have extents, not all extents are completely accurateTravis Roberts
1967, Resource Publication 41
No abstract available....
R. W. Imlay
1967, Professional Paper 573-B
G.H. Hughes
1967, Professional Paper 272-H
Don E. Wolcott
1967, Bulletin 1063-K
D.A. Myers
1967, Professional Paper 573-C
Neil Hotchkiss
1967, Resource Publication 44
No abstract available...
Edwin B. Eckel
1967, Professional Paper 545-B
The earthquake of March 27, 1964, wrecked or severely hampered all forms of transportation, all utilities, and all communications systems over a very large part of south-central Alaska. Effects on air transportation were minor as compared to those on the water, highway, and railroad transport systems. A few planes were...
N. F. Sohl
1967, Professional Paper 393-B
K. L. Wier
1967, Bulletin 1226
Walter O. Stieglitz, Richard L. Thompson
1967, Special Scientific Report - Wildlife 109
A.T. Miesch
1967, Professional Paper 574-A
Warren Hamilton, W. B. Myers
1967, Professional Paper 554-C
Don Price
1967, Water Supply Paper 1833
F. C. Boner, Frank Stermitz
1967, Water Supply Paper 1840-B
No abstract available....
Don Price
1967, Water Supply Paper 1847
The Eola-Amity Hills area ,comprises about 230 square miles on the west side of the Willamette Valley between Salem and McMinnville, Oreg. The area is largely rural, and agriculture is the principal occupation. Rocks ranging in age from Eocene to Recent underlie the area. The oldest rocks are a sequence...
Don Price
1967, Water Supply Paper 1839-I
F.T. Hidaka, Arthur Angus Garrett
1967, Water Supply Paper 1839-J
Hydrologic data collected in the Cedar and Snoqualmie River basins on the west slope of the Cascade Range have been analyzed to determine the amount of water lost by seepage from Chester Morse Lake and Masonry Pool and the. consequent gain by seepage to the Cedar and South Fork Snoqualmie...
B. L. Foxworthy, Charles T. Bryant
1967, Water Supply Paper 1594-E
Leon S. Hughes, Donald K. Leifeste
1967, Water Supply Paper 1839-A
The kinds and quantities of minerals dissolved in the surface water of the Neches River basin result from such environmental factors as geology, streamflow patterns and characteristics, and industrial influences. As a result of high rainfall in the basin, much of the readily soluble material has been leached from the...
Wayne A. Pettyjohn
1967, Water Supply Paper 1844
The Minot area is in the north-central part of North Dakota and includes part of the Souris River valley. The region is covered by glacial drift of late Wisconsin age except in small areas where the Fort Union Formation of Tertiary age crops out. Thickness of the drift is controlled...
Donald W. Fisher
1967, Water Supply Paper 1535-M
A 2-year study of precipitation composition over eastern North Carolina and southeastern Virginia has been completed. Chemical analyses were made of the major ions in monthly rainfall samples from each of 12 sampling locations. Areal and seasonal distributions were determined for chloride, calcium, magnesium, sodium, potassium, sulfate, and nitrate. Annual...
Donald L. Coffin, Clarence Albert Horr
1967, Water Supply Paper 1843
This report describes the geology and ground-water resources of that part of the Big Sandy Creek valley from about 6 miles east of Limon, Colo., downstream to the Kiowa County and Prowers County line, an area of about 1,400 square miles. The valley is drained by Big Sandy Creek and...
A.M. Moore
1967, Water Supply Paper 1819-K
Charles Franklin Keech, V. H. Dreeszen, Philip A. Emery
1967, Water Supply Paper 1839-F
York County, an area of 575 square miles, is situated on an upland plain in southeast Nebraska. Although tributaries of the Big Blue River have eroded valleys into this plain, much of the original surface is still intact and is characterized by broad shallow undrained depressions. The economy is based...