S.L. Grazis
1974, Open-File Report 74-1043
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Page 6182, results 154526 - 154550
Publication Extents
Not all publications have extents, not all extents are completely accurateR.G. Simpson
1974, Water-Resources Investigations Report 73-55
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2146
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2143
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2141
J. D. Peper
1974, Open-File Report 74-61
No abstract available....
Water Resources Division, U.S. Geological Survey
1974, Water Supply Paper 2147
Robert N. Oldale
1974, Geologic Quadrangle 1114
F. S. Simons
1974, IMAP 762
M. L. Sorensen, M. D. Crittenden Jr.
1974, Open-File Report 74-1
William M. Brown III, Lionel E. Jackson Jr.
1974, Miscellaneous Field Studies Map 625
Henry W. Roehler
1974, Geologic Quadrangle 1139
Roy H. Bingham, DeRoy L. Bergman, Wilbert O. Thomas Jr.
1974, Water-Resources Investigations Report 74-27
Heavy and intense rainfall of October 10 and 11, 1973, caused wide-spread flooding along many streams in north-central Oklahoma. This report shows the distribution and amounts of rainfall, and the magnitude and frequency of flood discharges at several sites in the area (sheet 1) and the extent of flooding in...
Water Resources Division, U.S. Geological Survey
1974, Water Data Report CT-73-1
Water Resources Division, U.S. Geological Survey
1974, Water Data Report WI-73-1-2
R.K. Gabrysch, C.W. Bonnet
1974, Open-File Report 74-123
The pumping of large amounts of ground water in the Houston-Galveston region, Texas, has resulted in water-level declines of as much as 200 feet (61 metres) in wells completed in the Chicot aquifer and as much as 325 feet (99 metres) in wells completed in the Evangeline aquifer during 1943-73....
E. H. Handman, J.B. Byrnes
1974, Miscellaneous Field Studies Map 487-D
E. J. McKay, M. J. Bergin
1974, Geologic Quadrangle 1145
Gerald F. Lindholm, J. O. Helgesen, W.L. Broussard, D.F. Farrell
1974, Hydrologic Atlas 490
The lower St. Croix River watershed is an elongate area of about 930 square miles bounded on the east by the St. Croix River. The St. Croix River forms the Minnesota-Wisconsin boundary along the eastern side of the watershed. Additional drainage to the St. Croix River includes areas of about 2,500...
Richard Van Horn, F.K. Fields
1974, IMAP 766-N
In the past man has built on land that might be covered by floodwaters, with little consideration of the consequences. The result has been disastrous to those in the path of floodwaters and has cost the loss of thousands of lives and untold billions of dollars in property damage in...
Richard Quintin Lewis, Alfred R. Taylor
1974, Geologic Quadrangle 1198
Donald L. Peterson
1974, Open-File Report 74-298
No abstract available. ...
Gerald F. Lindholm, J. O. Helgesen, W.L. Broussard, D.W. Ericson
1974, Hydrologic Atlas 488
Glacial drift overlies sedimentary, igneous, and metamorphic rocks in the Snake River watershed. The Snake River, which drains an area of about 1,030 square miles, originates in an extensive area of peat bogs in the northern part of the watershed. It flows southward across gently rolling glacial terrain in which the...
Harold E. McGovern, W.A. Long
1974, Hydrologic Atlas 517
No abstract available....
Don Price, Thomas E. Eakin
1974, Hydrologic Atlas 487
The Great Basin Region is defined to include the drainage of the Great Basin physiographic section (Fennman, 1931) in Idaho, Nevada, Utah, and Wyoming. In October 1966, the President’s Water Resources Council requested that a comprehensive framework study be made in the Great Basin Region under the leadership of the...