Water Resources Division, U.S. Geological Survey
1968, Open-File Report 69-292
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateEric G. Moore, Barry S. Wellar
1968, Open-File Report 68-187
George William Holmes
1968, Open-File Report 68-131
No abstract available....
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 624
No abstract available....
Robert Denny Trace, Thomas M. Kehn
1968, Geologic Quadrangle 742
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 621
No abstract available....
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 625
No abstract available....
1968, Open-File Report 68-41
No abstract available. ...
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 626
No abstract available....
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 637
No abstract available....
Robert M. Moxham
1968, Open-File Report 68-191
No abstract available....
Howard E. Simpson
1968, Geologic Quadrangle 756
Robert M. Moxham, Gordon W. Greene
1968, Open-File Report 69-176
Water Resources Division, U.S. Geological Survey
1968, Geophysical Investigations Map 629
No abstract available....
Water Resources Division, U.S. Geological Survey, U.S. Bureau of Mines
1968, Professional Paper 580
No abstract available....
1968, Open-File Report 68-59
No abstract available. ...
J. M. Hoare, W. H. Condon
1968, IMAP 523
William Stewart Eisenlohr, Charles E. Sloan
1968, Circular 558
This report presents all the information, obtained during the investigation, that lends itself to generalization. It describes conditions on that part of the Coteau du Missouri where there is little integration of drainage systems. The surface of the glacial drift in this region is dotted with shallow depressions known as...
John Phillip Schafer
1968, Geologic Quadrangle 712
J. Peter Trexler, Gordon H. Wood
1968, Geologic Quadrangle 701
H.P. Eisenhuth
1968, Circular 582
R. D. Cotter, L. E. Bidwell
1968, Hydrologic Atlas 269
The Lac qui Parle River watershed is underlain by thick water-bearing sections of glacial drift and Cretaceous rocks. Drainage is from the Coteau des Praries, a plateau in the southwest, to the Lac qui Parle reservoir, about 800 feet lower than the plateau. The term "watershed" as used in this...
Betty Skipp, Mary-Margaret Hepp
1968, Geologic Quadrangle 729
Jesse William Whitlow
1968, Open-File Report 68-326
Roy Newcome Jr., Donald E. Shattles, Carney P. Humphreys Jr.
1968, Water Supply Paper 1856
The potential for water-supply development in Harrison County is almost unlimited. During an average year, more than 350 billion gallons of water flow into the Gulf of Mexico from the streams of the county. With storage reservoirs these streams have a potential sustained supply of hundreds of millions of. gallons...