Norman P. Cuppels
1962, Open-File Report 62-35
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Publication Extents
Not all publications have extents, not all extents are completely accurateRobert Washburn Devaul, Bruce William Maxwell
1962, Hydrologic Atlas 27
J. S. Meyers, T. J. Nordenson
1962, Professional Paper 272-D
No abstract available....
G. E. Harbeck Jr.
1962, Professional Paper 272-E
Studies of evaporation made in recent years nave provided values of the mass-transfer coefficient, N, in the equation E=Nut(e0—ea) for reservoirs having surface areas ranging from 1 to nearly 30,000 acres. The apparent correlation of N with reservoir surface area may in large part be associated with variations in the...
John Charles Miller
1962, Bulletin 1031-E
J. D. Vine
1962, Professional Paper 356-D
William B. Bull
1962, Open-File Report 62-17
E.S. Simpson
1962, Professional Paper 411-C
Stuart L. Schoff
1962, Open-File Report 73-254
Donald Eldon Trimble, Wilfred James Carr
1962, Open-File Report 62-135
Frederick Otto Simon
1962, Open-File Report 62-126
Rhenium is determined by spectrophotometry of the tellurium sol formed by the reduction of tellurate by stannous chloride under the catalytic influence of rhenium. A detailed investigation of the conditions for high sensitivity and stability at lowest concentration levels of rhenium is presented as well as the behavior of twenty-six...
Joel S. Watkins, Zvi Yuval
1962, Open-File Report 62-150
George Plafker
1962, Bulletin 1031-F
Charles W. Lane, E.L. Reavis, Gilbert J. Stramel
1962, Hydrologic Atlas 58
Donald W. Peterson
1962, Miscellaneous Field Studies Map 253
No abstract available....
W. R. Griffitts, R. G. Yates, W.C. Overstreet
1962, Miscellaneous Field Studies Map 252
Sam H. Patterson, John W. Hosterman, John Warfield Huddle
1962, Bulletin 1122-F
The Haldeman and Wrigley 7th-minute quadrangles are near the western edge of the eastern Kentucky coal field and cover an area of approximately 117 square miles in parts of Carter, Rowan, Elliott, and Morgan Counties, Ky. The rocks exposed in the two quadrangles are of Early and Late Mississippian and...
William Gamewell Pierce, Ernest Isaac Rich
1962, Bulletin 1148
No abstract available....
L.L. Laine, J.J. Murphy
1962, Open-File Report 62-162
Annual discharge from Beaver Creek basin is estimated to have averaged 217,000 acre-feet during a 19-year base period, water years 1938-56, equivalent to an average annual runoff depth of 4.7 inches over the 857 square-mile drainage area. About 55,000 acre-feet per year comes from Little Beaver Creek basin, a tributary...
Charles Franklin Keech
1962, Bulletin 1133-B
No abstract available....
Glenn R. Scott
1962, Bulletin 1121-L
D.L. Healey, Carter H. Miller
1962, Trace Elements Investigations 827
Harold Julius Hyden, Walter Danilchik
1962, Bulletin 1147-B
William Clarence Walton
1962, Water Supply Paper 1609
Camas Prairie is an eastward-trending intermontane basin along the north flank of the Snake River Plain in southern Idaho. The basin is about 40 miles long and averages about 8 miles wide. It was formed as a structural depression in which a considerable thickness of alluvial and lake deposits accumulated...
Carl Maurice Bunker, Marvin D. Shutler
1962, Trace Elements Investigations 832