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Publications

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: 3291

An appraisal of ground water for irrigation in the Wadena area, central Minnesota An appraisal of ground water for irrigation in the Wadena area, central Minnesota

The Wadena area is part of a large sandy plain in central Minnesota whose soils have low water-holding capacity. Drought conditions which adversely affect plant growth frequently occur in the summer when moisture is most needed. To reduce the risk of crop failure in the area supplemental irrigation is on the increase. This study was made to evaluate the ground-water resources of the area...
Authors
F.G. Lindholm

Sediment problems in urban areas Sediment problems in urban areas

A recognition of and solution to sediment problems in urban areas is necessary if society is to have an acceptable living environment. Soil erosion and sediment deposition in urban areas are as much an environmental blight as badly paved and littered streets, dilapidated buildings, billboard clutter, inept land use, and air, water, and noise pollution. In addition, sediment has many...
Authors
Harold P. Guy

Water resources of the Wild Rice River watershed, northwestern Minnesota Water resources of the Wild Rice River watershed, northwestern Minnesota

The Wild Rice watershed includes two general physiographic areas- the glacial Lake Agassiz Plain and a glacial moraine. The lake plain is extremely flat in the western part, sloping only a few feet per mile, but in the eastern part the plain is traversed in a north-south direction by long, narrow beach ridges up to 20 feet high. The moraine is an area of hills and depressions. The local...
Authors
Thomas C. Winter, L. E. Bidwell, Robert W. Maclay

Geology and ground-water resources of the Grand Rapids area, north-central Minnesota Geology and ground-water resources of the Grand Rapids area, north-central Minnesota

This report is one of a series of studies of geology and ground-water availability conducted in and near selected communities on the Mesabi Iron Range, north-central and northeastern Minnesota. This report describes the geology and ground-water conditions in the 303 square-mile Grand Rapids area.
Authors
Edward L. Oakes

Water resources of the Redwood River watershed, southwestern Minnesota Water resources of the Redwood River watershed, southwestern Minnesota

The Redwood River watershed contains 739 square miles underlain by glacial drift and sedimentary and crystalline rocks. The land surface slopes gently northeastward and eastward from altitudes greater than 1900 feet at the southwestern edge to less than 850 feet at the mouth of the Redwood River in the east. The area has slight local relief shaped by continental glaciation. The Redwood...
Authors
Wayne A. Van Voast, L.A. Jerabek, R.P. Novitzki

Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula

The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, and trout fishing), but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to...
Authors
G. E. Hendrickson, C. J. Doonan

Water resources of the River Rouge basin, southeastern Michigan Water resources of the River Rouge basin, southeastern Michigan

The River Rouge basin is characterized by moderately hilly topography to the northwest graduating to a relatively level land surface to the south east. Stream gradients near the northwestern basin divide are relatively steep; but many become more steep in reaches where they cross beach lines of former glacial lakes. In the lower reaches of the River Rouge gradients lessen.
Authors
R. L. Knutilla
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