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Browse more than 150,000 publications authored by our scientists over the past 100+ year history of the USGS.  Publications available are: USGS-authored journal articles, series reports, book chapters, other government publications, and more.

Upper Midwest Environmental Sciences Center Publications

Filter Total Items: 3323

Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota

The water resources were studied within an area whose natural ground-water flow is largely towards the center of the metropolitan area. This area coincides with the extent of the Hinckley Sandstone aquifer. Thus, the general geohydrology of the area bounded by the extent of the Hinckley Sandstone (about 6,000 square miles) as it relates to the hydrology of the Minneapolis-St. Paul...
Authors
R.F. Norvitch, T.G. Ross, Alex Brietkrietz

Water resources of Wisconsin, Pecatonica-Sugar River basin Water resources of Wisconsin, Pecatonica-Sugar River basin

The purpose of this report is to describe the physical environment, availability, characteristics, distribution, movement, and quailty of water in the Pecatonica-Sugar River basin. In addition, water use and water problems are summarized to give an understanding of man's management of water within the basin.
Authors
S. M. Hindall, Earl L. Skinner

Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan

The Tri-County region, consisting of Clinton, Eaton, and Ingham Counties, is an area of 1,697 square miles in Michigan's Lower Peninsula and has as its hub the Lansing metropolitan area. The land surface ranges in altitude from about 700 to about 1,000 feet. The region receives an average of about 31 inches of precipitation each year. The population is nearing 400,000 and by 1990 will be...
Authors
Kenneth Eugene Vanlier, Warren W. Wood, Jilann O. Brunett

Relation of channel slope to reaeration of Michigan streams Relation of channel slope to reaeration of Michigan streams

Reaeration coefficients (k2), which are rate constants for the process of oxygen absorption from the atmosphere, have been computed for Michigan's streams using an equation developed by Bennett and Rathbun (1972). Mean velocity and mean depth data, which are necessary for the computation, have been extracted from discharge measurements made at gaging stations throughout the State. The...
Authors
T. Ray Cummings

Glacial and postglacial geologic history of Isle Royale National Park, Michigan Glacial and postglacial geologic history of Isle Royale National Park, Michigan

Isle Royale was overridden by glacial ice during each of the four major glaciations of the Pleistocene Epoch, and each successive glaciation essentially obliterated all direct evidence of preceding glaciations on the island. In the waning phase of the last major glaciation, the Wisconsin Glaciation, the frontal ice margin retreated northward from at least the greater part of the Lake...
Authors
N. King Huber

Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota

Stratified fluvial sediments occur within the glacial drift at many places in the Mesabi Iron Range area. These sediments, which are important aquifers, occur extensively between the three main till units. The thickest and most extensive aquifer consists of glaciofluvial sediments that lie between the surficial till and the middle till unit, the bouldery till. Thickness of the...
Authors
Thomas C. Winter

Appraisal of ground water for irrigation in the Little Falls area, Morrison County, Minnesota Appraisal of ground water for irrigation in the Little Falls area, Morrison County, Minnesota

Anticipated irrigation on sandy soils has prompted evaluation of ground-water supply potential in the Little Falls area. Geologic conditions cause ground-water availability to vary widely in the area. The largest and most readily available groundwater source is the glacial outwash sand and gravel from which the soils were derived. Test augering shows that the saturated surficial outwash...
Authors
John O. Helgesen
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