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165549 results.

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Page 5797, results 144901 - 144925

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Reconnaissance of the Red Lake River, Minnesota
Lev Ropes, Richmond F. Brown, D.E. Wheat
1969, Hydrologic Atlas 299
This report is intended to serve a wide range of people including educators, scientists, planners, and those who wish to enjoy travel on the river. the data-summary charts, graphs, and tables are intended to be specific enough so that users who require precise information need not resynthesise the original numerical...
Ground-water resources of the St. James area, South-central Minnesota
L.H. Ropes
1969, Hydrologic Atlas 334
The purpose of this investigation was to evaluate the quality and quantity of the ground-water resources in the area of St. James, Minnesota. St. James is located in the center of Watonwan County in south-central Minnesota. The area is covered by a thick layer of glacial drift which is underlain...
Water resources of the Belle River basin, southeastern Michigan
R. L. Knutilla
1969, Hydrologic Atlas 317
This hydrologic atlas represents a part of a comprehensive study of the water resources of southeastern Michigan. The purpose of the atlas is to present data on (1) the physical features of the Belle River and its tributaries, (2) the characteristics of streamflow, (3) the quality of ground and surface...
Water resources of the Otter Tail River Watershed, West-central Minnesota
Thomas C. Winter, L. E. Bidwell, R.W. Maclay
1969, Hydrologic Atlas 296
The Otter Tail River watershed includes three general physiographic areas- a moraine and ice-contact area, an outwash plain, and the plain of Glacial Lake Agassiz. The moraine and ice-contact area is a fairly rugged complex of hills characterized by local relief of several hundred feet in some areas, particularly in the...
Water resources of the Buffalo River Watershed, West-central Minnesota
Robert W. Maclay, L. E. Bidwell, Thomas C. Winter
1969, Hydrologic Atlas 307
The Buffalo River watershed includes two general physiographic areas – a glacial lake plain and an glacial moraine. The lake plain, which was formed by Glacial lake Agassiz more than 9,000 years ago, is extremely flat – sloping only a few feet per mile westward near the Red River of the...
Water resources of the Pine River Basin, southeastern Michigan
R. L. Knutilla
1969, Hydrologic Atlas 327
The land surface of the Pine River basin, an area of 194 square miles, is a relatively flat or gently undulating northwest to southeast trending glacial lake plain.The plain is interrupted by small streams and by a series of former glacial lake beaches. Other irregularities are the morainal hills in...