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Page 5713, results 142801 - 142825

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Not all publications have extents, not all extents are completely accurate
Field trip guidebook to the hydrogeology of the Rock-Fox River basin of Southeastern Wisconsin
C. L. R. Holt Jr., R. D. Cotter, J. H. Green, P. G. Olcott
1970, Wisconsin Geological & Natural History Survey Information Circular 17
On this trip we will examine some hydrogeologic characteristics of glacial features and emphasize ground-water management within the Rock-Fox River basin. Field stops will include the hydrogeology of a classical glacial terrane--the Kettle moraine--and the management of ground-water resources for industrial, municipal, agricultural, and fish-culture purposes. Descriptions of the geology,...
A test of flushing procedures to control salt-water intrusion at the W. P. Franklin Dam near Ft. Myers, Florida and The magnitude and extent of salt-water contamination in the Caloosahatchee River between La Belle and Olga, Florida
Durward H. Boggess
1970, Information Circular 62
During low-flow periods, salty water from the tidal part of the Caloosahatchee River moves upstream during boat lockages at the W. P. Franklin Darn near Ft. Myers, Florida, as shown on figure L Salty water enters the lock chamber through openings of the downstream sector gates which separate tidal and...
Statistical summaries of New Jersey streamflow records
Stanley L. Laskowski
1970, New Jersey Division of Water Policy and Supply Water Resources Circular 23
In 1961 the U.S. Geological Survey prepared a report which was published by the State of New Jersey as Water Resources Circular 6, "New Jersey Streamflow Records analyzed with Electronic Computer" by Miller and McCall. Basic discharge data for periods of record through 1958 were analyzed for 59 stream-gaging stations...
Geology and ground water resources, Williams County, North Dakota
Theodore F. Freers, C. A. Armstrong
1970, North Dakota Geological Survey Bulletin 48
Williams County, in northwestern North Dakota, is located near the center of the structural and sedimentary Williston basin. The preglacial sedimentary formations beneath the county are as much as 14,828 feet thick. Their beds dip generally to the south except along the flanks of the north-south striking Nesson anticline in...