Rates of Runoff for the Design of Conservation Structures in the Upper Mississippi Valley Upland Loessial Areas (Classic Reprint) - Softcover

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Excerpt from Rates of Runoff for the Design of Conservation Structures in the Upper Mississippi Valley Upland Loessial Areas

The Carrington soils are derived from friable glacial till. They have dark-colored surface layers like the Tama and Dodgeville soils and are deep and moderately per meable. Within this area records of runoff available as a basis for design of conser vation structures and practices on small drainage. Basins are limited to those obtained by the Soil Conservation Service at La Crosse and Fennimore, Wis., and the Ralston Creek cooperative project of the State University of Iowa, Department of Agriculture, and the United States Geological Survey. Records obtained from these studies include.

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