Lawrence C. Rowan, John Francis McCauley, Esther A. Holm
1969, Open-File Report 69-235
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Page 5790, results 144726 - 144750
Publication Extents
Not all publications have extents, not all extents are completely accurateGeorge Joseph Neuerburg
1969, Open-File Report 69-182
Maxwell E. Gardner
1969, Open-File Report 69-102
No abstract available....
Fred Peterson
1969, Open-File Report 69-202
Upper Cretaceous strata in the southeastern Kaiparowits region of south-central Utah consist of approximately 3,500 feet of interfingering sandstone, mudstone, shale, and coal in the Dakota Formation (oldest), Tropic Shale, Straight Cliffs Formation, and Wahweap Formation (youngest). The formations consist of several depositional facies that can be recognized by characteristic...
Peter M. Gerrild, Robert Joseph Lantz
1969, Open-File Report 69-105
L. E. Garrison
1969, Open-File Report 69-103
Donald L. Peterson
1969, Open-File Report 69-200
Donald Parker Elston, Charles R. Willingham
1969, Open-File Report 69-91
Richard A. Minnich, Leonard W. Browden, Robert W. Pease
1969, Open-File Report 69-172
Donald L. Peterson
1969, Open-File Report 69-201
Raymond L. Elliott, Thomas P. Miller
1969, Open-File Report 69-89
Lee J. Eicher, A.R. Myers
1969, Open-File Report 69-88
Robert H. Mullens Jr., Leslie W. Senger
1969, Open-File Report 69-178
Thomas P. Miller
1969, Open-File Report 69-169
No abstract available....
David Carl Hedlund, George Sutter Corchary
1969, Open-File Report 69-125
Thomas P. Miller, Leonard A. Anderson
1969, Open-File Report 69-170
John R. Ege, R. D. Carroll, R.J. Way, J. E. Magner
1969, Open-File Report 69-87
USBM/AEC Colorado Core Hole No. 3 (Bronco BR-1) is located in the SW1/4SW1/4SW1/4 sec. 14, T. 1 N., R. 98 W., Rio Blanco County, Colorado. The collar is at a ground elevation of 6,356 feet. The hole was core drilled between depths of 964 and 3,325 feet with a total...
A.T. Edgerton, D.T. Trexler, S. Sakamoto, J.E. Jenkins
1969, Open-File Report 69-86
Joseph P. Beverage, Milton N. Swecker
1969, Water Supply Paper 1873-B
Improved management of the water resources of Grays Harbor, Wash., requires more data on the water quality of the harbor and a better understanding of the influences of industrial and domestic wastes on the local fisheries resources. To provide a more comprehensive understanding of these influences, the U.S. Geological Survey...
Winchell Smith
1969, Water Supply Paper 1877
A reliable measure of the fresh-water outflow from the Sacramento-San Joaquin delta is needed for the operation of the California Water Project and for the evaluation of the interrelated water problems of the delta and San Francisco Bay regions. The Chipps Island channel, immediately downstream from the confluence of the...
H.E. Gill
1969, Water Supply Paper 1757-K
This report gives a general summary of the availability and use of ground water and describes the occurrence of ground water in five major geohydrologic provinces lying in the eight administrative regions of Ghana. The identification and delineation of the geohydrologic provinces are based on their distinctive characteristics with respect...
S. G. Brown, Herbert H. Schumann
1969, Water Supply Paper 1859-F
The Willcox basin is an area of interior drainage in the northern part of Sulphur Springs Valley, Cochise and Graham Counties, Ariz. The basin comprises about 1,500 square miles, of which the valley floor occupies about 950 square miles. The basin probably formed during middle and late Tertiary time, when...
Philip M. Cohen, O. Lehn Franke, N. E. McClymonds
1969, Water Supply Paper 1879-F
John J. Hickey
1969, Water Supply Paper 1879-E
Graphs and a table are presented showing the variations in streambed elevations that have occurred over the years in the low-water channels at selected gaging stations in northwestern California. The streambed elevations are calculated from data obtained during discharge measurements. The greatest elevation changes that were recorded occurred between the...
K. J. Takasaki, Santos Valenciano
1969, Water Supply Paper 1874
The Kahuku area comprises the north end of the Koolau Range and its bordering coastal plain. This part of the range is less deeply eroded than oth3r parts, and except for long, narrow valleys and cliffs near the shore, it has retained the general shape of the original volcanic dome....