K. J. Murata, D.H. Richter
1966, Professional Paper 537-A
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Publication Extents
Not all publications have extents, not all extents are completely accurateDivision Of Wildlife Research
1966, Wildlife Leaflet 474
K.O. Emery
1966, Professional Paper 529-A
A. E. Roberts
1966, Professional Paper 526-B
A.C. Lendo
1966, Water Supply Paper 1586-E
L.C. Dutcher, H. E. Thomas
1966, Water Supply Paper 1757-E
C.M. Hoffman, G.L. Stewart
1966, Water Supply Paper 1696-D
Herman John Koloseus, Jacob Davidian
1966, Water Supply Paper 1592-C,D
Marvin J. Fishman, Sanford C. Downs
1966, Water Supply Paper 1540-C
This manual describes atomic-absorption-spectroscopy methods for determining calcium, copper, lithium, magnesium, manganese, potassium, sodium, strontium and zinc in atmospheric precipitation, fresh waters, and brines. The procedures are intended to be used by water quality laboratories of the Water Resources Division of the U.S. Geological Survey. Detailed procedures, calculations, and methods...
Thad Gerald McLaughlin
1966, Water Supply Paper 1805
Philip M. Cohen
1966, Water Supply Paper 1816
Most of the work of the interagency Humboldt River Research Project in the Winnemucca reach of the Humboldt River valley has been completed. More than a dozen State and Federal agencies and several private organizations and individuals participated in the study. The major objective of the project, which began in...
Benjamin L. Jones
1966, Water Supply Paper 1532-C
Analyses of data collected from two small basins in northern Pennsylvania during the period May 1954 to September 1960 indicated that changes in land use and land treatment have affected suspended- sediment discharge from the basins. Extensive land use and land-treatment changes have taken place in the 12.2-square-mile Corey Creek...
Harry H. Barnes, Harold G. Golden
1966, Water Supply Paper 1674
No abstract available....
Walter B. Keighton
1966, Water Supply Paper 1586-G
Sustained flows of fresh water greater than 3,500, 4,400, and 5,300 cubic feet per second into the Delaware River estuary at Trenton, NJ assure low salinity at League Island, Eddystone, and Marcus Hook, respectively. When the discharge at Trenton is less than these critical values, salinity is very sensitive to...
1966, Water Supply Paper 1822
Increasing world activity in water-resources development has created an interest in techniques for conducting investigations in the field. In the United States, the Geological Survey has the responsibility for extensive and intensive hydrologic studies, and the Survey places considerable emphasis on discovering better ways to carry out its responsibility. For...
J.R. Randolph, Ruth G. Deike
1966, Water Supply Paper 1863
G.A. Miller, R. E. Evenson
1966, Water Supply Paper 1819-A
Overdraft in the Santa Maria Valley ground-water basin since about 1946 has resulted in a significant decline in water levels throughout the basin as ground water has been removed from storage. In 1959 approximately 2,200,000 acre-feet of ground water was in storage above sea level in the ground-water reservoir. Estimates...
S. K. Love
1966, Water Supply Paper 1946
Edwin Allen Bell
1966, Water Supply Paper 1819-C
Water problems and their solutions have been associated with the growth and development of the Louisville area for more than a century. Many hydrologic data that aided water users in the past can be applied to present water problems and will be helpful for solving many similar problems in the...
J. C. Mundorff, K.M. Waddell
1966, Water Supply Paper 1819-H
The Little Blue River drains about 3,37)0 square miles in south-central Nebraska and north-central Kansas. The uppermost bedrock in the basin is limestone and shale of Permian age and sandstone, shale, and limestone of Cretaceous age. Bedrock is exposed in many places in the lower one-third of the basin but...
J. C. Mundorff
1966, Water Supply Paper 1798-C
R.O.R. Martin, Ronald L. Hanson
1966, Water Supply Paper 1838
This report summarizes the storage capacities and related data of reservoirs and controlled natural lakes for the contermimous United States, Alaska, Hawaii, and the Commonwealth of Puerto Rico. Data are given for all storage facilities having a usable capacity of 5,000 acre-feet or more and completed or under construction as...
Stanley Eugene Norris, Andrew Maute Spieker
1966, Water Supply Paper 1808
The principal aquifers of the Dayton area are sand and gravel layers in the 150- to 250-foot thick glacial deposits filling the river valleys (Miami River and its tributaries), which were originally cut in bedrock by preglacial streams. The upper and lower aquifers are separated by a poorly permeable till-rich...
John T. Gallaher, William Evans Price
1966, Water Supply Paper 1818
Marlin E. Lowry, T. Ray Cummings
1966, Water Supply Paper 1807
Sheridan County is in the north-central part of Wyoming and is an area of about 2,500 square miles. The western part of the county is in the Bighorn Mountains, and the eastern part is in the Powder River structural basin. Principal streams are the Powder and Tongue Rivers, which are...