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Publications

These publications are written or co-authored by Central Midwest Water Science Center personnel in conjuction with their work at the USGS and other government agencies.  They include USGS reports, journal articles, conference proceedings, and published abstracts that  are available in the USGS Publications  Warehouse.

Filter Total Items: 938

The 1965 Mississippi River flood in Iowa

The great flood of 1965 on the Mississippi River, along the eastern border if the State, exceeded any flood known in 139 years. It cause damages probably in excess of ten millions of dollars in the State of Iowa. Studied now in progress will more thoroughly cover this and other phases of the flood. The underlying cause of the flood was an abnormally cold winter which prevented the melting of an ex
Authors
Harlan H. Schwob, Richard E. Myers

The water story in Central Iowa

"The general welfare of the people of the state of Iowa requires that the water resources of the state be put to beneficial use to the fullest extent of which they are capable."  This can be achieved only by a knowledge and understanding of the water resources - their use, their source, their quality, their availability, and the demands place upon them.  To provide such knowledge and understanding
Authors
F. R. Twenter, R. W. Coble

Water resources of the English River, Old Mans Creek, and Clear Creek basins in Iowa

The surface and ground water resources of a 991 square mile area comprising the drainage basins of English River, Old Mans Creek and Clear Creek are presented. These basins lie to the west and southwest of Iowa City, Iowa, and all three streams are tributary to the Iowa River. The area is comprised of rolling uplands with relatively broad valleys and is devoted mainly to agriculture and livestock
Authors
H.H. Schwob

Cedar River basin floods

No abstract available
Authors
Harlan H. Schwob

Geology and ground-water resources of Clayton County, Iowa

Clayton County includes 784 square miles in northeastern Iowa and in 1960 had a population of 21, 962.  For the most part, the county is a dissected upland that is drained mainly by the southeastward flowing Turkey River and its principal tributary, the Volga River.  The Turkey River empties into the Mississippi River, which flows southward along the eastern border of the county.  The climate is h
Authors
W. L. Steinhilber, O. J. Van Eck, A.J. Feulner

Low-flow characteristics of Iowa streams

Study of the occurrence of low flow on interior Iowa streams and the Big Sioux River.
Authors
Harlan H. Schwob

Drainage areas of Iowa streams

The drainage area of a stream at a specified location ordinarily may be defined as that area, measured in a horizontal plane, which is enclosed by a topographic divide such that direct surface runoff from precipitation would drain by gravity into the river basin above the specified point. One of the most important factors in the hydrologic computation for the design of structures on or over waterc
Authors
O.J. Larimer

Geology and ground-water resources of Webster County, Iowa

Webster County, comprising an area of 718 square miles just northwest of the center of Iowa, had a population of 44,241 in 1950, with 25,115 in Fort Dodge, the principal city. Some 94.4 percent of the county is in farm land; corn is the principal crop and is used in the raising of hogs and cattle, an important oc cupation in this part of the country. Mineral products include gypsum, clay, coal, sa
Authors
William E. Hale