Publications
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Upper Midwest Environmental Sciences Center Publications
Filter Total Items: 3223
Floods in Wisconsin: Magnitude and frequency
Flood data from gaging stations on Wisconsin rivers and streams are listed in this report. From these data, composite frequency curves were defined which express the ratio of floods of various recurrence intervals to the mean annual flood. Multiple correlation techniques were used to obtain formulas that relate the basin parameters of drainage area, main channel slope, and lake and reservoir surfa
Authors
D.W. Ericson
Some aspects of the effect of urban and suburban development upon runoff
No abstract available.
Authors
Sulo Werner Wiitala
Availability of ground water in Lyon County, Minnesota
Lyon County is in southwestern Minnesota, about 150 miles southwest of Minneapolis and St. Paul The basement rocks in the area consist of granite and quartzite of Precambrian age. These materials are in turn overlain by shale and sandstone of Cretaceous age, glacial drift of Pleistocene age, and alluvium of Recent age. Ground water is available primarily from aquifers in Pleistocene and Cretaceous
Authors
Harry G. Rodis
Aquifers in melt-water channels along the southwest flank of the Des Moines Lobe, Lyon County, Minnesota
During the Gary and Mankato substages of Wisconsin glaciation the Des Moines lobe advanced southeastward through the broad lowland of the Minnesota River valley of southwestern Minnesota, and thence southward to central Iowa.
Among the most prominent topographic features in Lyon County, Minn., are five southeastward-trending end moraines, two of which are associated with and parallel to belts of s
Authors
Robert Schneider, Harry G. Rodis
Exploratory drilling for ground water in the Mountain Iron-Virginia area, St. Louis County, Minnesota
The Mountain Iron-Virginia area is a broad, southwest-trending valley in the central part of the Mesabi Range. The valley, which heads in the Laurentian Divide, and covers about 120 square miles, coincides approximately with a bedrock valley filled with as much as 150 feet of glacial deposits.
A complex sequence of glacioaqueous sediments made up of clay, silt, sand, and gravel was delineated from
Authors
R. D. Cotter, J.E. Rogers
The trout fishery in Shenandoah National Park
Populations of brook trout in streams of Shenandoah National Park were reduced drastically early in the past decade by a succession of unusually severe droughts and floods. The drying of stream beds, predation, and scouring were principal factors in the loss of fish. The park was closed to fishing in 1954 and 1955 to protect survivors. The small numbers of survivors quickly repopulated the streams
Authors
Robert E. Lennon
Blood properties of prespawning and postspawning anadromous alewives (Alosa pseudoharenqus)
Abstract has not been submitted
Authors
C.J. Sindermann, D.F. Mairs