Laserfiche WebLink
<br />CHRISTOPHER M. KAVANAUGH 5 <br /> <br />Minnesota River Basin Assessment Project <br /> <br />by <br /> <br />Christopher M. Kavanaugh <br /> <br />Minnesota Department of Natural Resources <br />Section of Fisheries <br />20596 Highway 7 <br />Hutchinson, Minnesota 55350 <br /> <br />Abstract. The Minnesota River basin encompasses 44,300 km2 in southwestem <br />Minnesota, eastem South Dakota, and north-central Iowa. The river flows 597 km to its <br />confluence with the Mississippi River at St. Paul, Minnesota. Original vegetation in the <br />basin was tall grass prairie, prairie wetlands, and hardwood forests. Agriculture <br />dominates the land use throughout the basin. The Minnesota River has a negative effect <br />on water quality in the Mississippi River with regard to sediment and nutrients. The fish <br />community in the basin is composed of 84 native and 4 introduced species. The river <br />supporls a sport fishery for walleye (Stizostedion vitreum), channel catiJSh (lctalurus <br />punctatus), northem pike (Esox lucius), and flathead catfish (Pylodictis olivaris). A <br />commercial fishery exists for common carp (Cyprinus carpio), buffalo (lctiobus spp.), and <br />freshwater drum (Aplodinotus gro,nniens). Fish consumption advisories for PCB's are in <br />place for most species. Restoration planning began in 1989 with the initiation of the <br />Minnesota River Assessment Project. The project is funded primarily by the Minnesota <br />State Legislature through the Legislative Commission on Minnesota Resources. The <br />Minnesota River Assessment Project is a multidisciplinary investigation of the physical, <br />chemical, biological, and land-use characteristics of the basin with the goal of <br />recommending Best Management Practices (BMPs) to achieve water quality goals. <br />Implementation of recommendations will be directed by a citizens advisory committee <br />made up of 30 individuals with diverse backgrounds. The citizens advisory committee <br />will target its efforts at addressing runoff and sedimentation. <br /> <br />The Minnesota River is the largest tributary to <br />the Mississippi River in Minnesota. The river be- <br />gins at the South Dakota-Minnesota border and <br />flows 597 km before emptying into the Mississippi <br />River at St. Paul, Minnesota (Fig. 1). Average gra- <br />dient in the stream is 0.2 m/km. The entire basin <br />covers about 44,300 km2 in Minnesota, South Da- <br />kota, and Iowa. <br />The Minnesota River is often referred to as Min- <br />nesota's "forgotten river" and is described as a <br />resource in trouble, which is far different from the <br />descriptions provided by early explorers. In the <br />1770's, J. Carver (1776) described the river as "most <br />delightful country abounding with all the necessar- <br />ies of life that grow spontaneously." In 1823, W. <br />Keating (1825) described the river bed as "chiefly <br />white sand," implying the water was clear enough <br />to see bottom. In the 1830's, Featherstonaugh (1970 <br /> <br />reprint) 'travelled the river, known then as the <br />Minnay Sotor by the Sioux. He commented on the <br />vast areas of wetlands he was able to see while <br />paddling. Today that would be nearly impossible <br />given the.deeply cut vertical banks. <br /> <br />Geologic Characteristics <br /> <br />The Minnesota River is small compared with its <br />expansive valley, nearly 8 km wide and 90 m deep <br />in places. The river valley was carved by Glacial <br />River W 8.1TEln as it discharged from the south end <br />of Glacial Lake Agassiz. As the elevation of Lake <br />Agassiz dropped, a very small ridge appeared at <br />Browns Valley, Minnesota, which became a conti- <br />nental divide. To the north the Red River of the <br />North flows to Hudson Bay, and to the south the <br />Minnesota River flows to the Mississippi River. <br />