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<br /> <br />,d many additional activities are avall- <br />I Vermillion Lake, which receives a <br />IX of visitors from the SioUIX Falls met- <br />lrea. Basin residents go down to the <br />liver for boating, swimming, camp- <br />picnicking because recreation <br />and access are more readily avail- <br />than along the Vermillion River. <br /> <br />operations, and some is suffered by the small <br />towns that dot the farming landscape. <br />It is commonly believed that flooding in <br />the Basin is getting worse, but there is really <br />no way to compare present conditions to floods <br />that occurred 15, 50, or 200 years ago. In all <br />probability, some human activities have con- <br />tributed to the flood problem-unsuitable <br /> <br />lion Dam was built on the East Fork to provide <br />irrigation and recreation, but it has little flood <br />control capacity. Several smaller dams have <br />been built on the forks and tributaries of the <br />Vermillion River, mostly to impound water <br />rather than to control flooding. In 1983 the <br />U.S. Soil Conservation Service finished a plan <br />for improvements in the Turkey and Clay <br /> <br /> <br />@ITUATION <br /> <br />,dies of water; the Vermillion River <br />overflows its banks from time to <br />, results in acute and chronic flood- <br />, typical of many rural, agricultural <br />Dughout the country. The low topo- <br />lief, local land use practices; the rates <br />ation, evaporation, transpiration, and <br />eeze/thaw cycles, and groundwater <br />:ontribute to the intensity of floods. <br />waters inundate farmlands, impede <br />al drainage an,! community storm- <br />off, damage roads, and enter homes <br />esses. Measured in monetary terms, <br />he damage is done to agricultural <br /> <br />land use practices, people living in the river's <br />floodplains and low areas, and natural flood <br />storage areas (wetlands) that have been <br />drained, for example. It is also possible that a <br />meteorological "wet cycle" is taking place. <br />Probably the true "cause" is some combination <br />of all these things, and others. <br />Over the past few decades, many attempts <br />have been made to alleviate the flooding in the <br />Vermillion Basin; many other ideas have been <br />suggested but not adopted or carried out. The <br />river has been channelized from about 11 miles <br />below Centerville to 2 miles above Vermillion. <br />There are over 50 miles oflevees on both sides <br />of the lower Vermillion River from Vermillion <br />to about 2 miles above Long Creek. East Vennil- <br /> <br />. <br /> <br />Creek watersheds in the lower part of the <br />Basin, but it was not implemented because <br />there was no local sponsorship. In 1987 the <br />Corps of Engineers began a 5-year study of <br />Basin flooding, but no cost-effective solutions <br />that met the Corps' criteria were found. <br />At the same time, the residents' concern <br />about other water-related issues has been grow- <br />ing, too. The U.S. Geological Survey and the <br />South Dakota Geological Survey examined the <br />quantity and quality of groundwater in Turner <br />County in 1990. The Statewide Comprehensive <br />Outdoor Recreation Plan, completed in 1992, <br />outlined ways to handle growing pressure on <br />South Dakota's recreational resources, espe- <br />cially lakes, streams, and wetlands. The area is <br /> <br />