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R�solution No. /G'�7 <br /> � Page 7 , <br /> 6 . A 1971 PCA study by Narza Engineering Company, Barr <br /> Engineering Company, Eugene Hickock and Associates, and the <br /> University of Minnesota Limnological Research Center concluded ." <br /> that Lake rSinnetonka was being subject to accelerated eutrophication <br /> caused by existing and increasing urbanization of the watershed <br /> and consequent increasing inputs of nutrient elements including <br /> phosphorus and nitrogen. <br /> 7 . Orono Ordinance No. 213, The Flood Plain and Wetlands <br /> Ma�agement Ordinance, adopted October 26, 1978, references and <br /> adopts the October 17, 1978 HUD Flood Insurance Study which had <br /> been ongoing since rlarch, 1974. This study and Ordinance <br /> identifies the following in regards to Stubbs Bay (see Exhibit F) . <br /> � . -Ordinary high water elevation: . 929 . 4 ft. MSL <br /> -Regulatory flood protection elevation: 932 . 5 ft. MSL <br /> -Special flood hazard areas caused by tributary � <br /> . to Stubbs Bay (includes Marina property) : <br /> Flood hazard zone A-2 (below) 931. 0 ft. MSL <br /> • Sheet flow area ( lft, depth) zone A-0 (below) 935. 0 ft. MSL <br /> -Regulatory flood protection elevation: �1 ft, above ground <br /> � level but not less than 932.5 ft. MSL <br /> B. NATURAL LAND FEATURES <br /> - . 1. The Study Area topography is of two basic types . The land <br /> near the Bay is relatively flat including some marshland and <br /> flood prone areas . T'he flat areas extend from the shoreline <br /> � back several hundred feet in some areas , notably the large marsh . <br /> along the northwest tributary- to the bay. The remaining land is <br /> gently rolling to steep slopes rising 30 to 40 feet above lake _ <br /> level. Slopes range above 100% along the northeast tributary <br /> creek, 50-100% between West Lake S_treet and Tonkawa Road and <br /> 5-20% t�ihere most of the residencest'are constructed. <br /> 2. The Study Area soils range from Marsh, Lake Beaches and <br /> ' Hamel loams in the marshy areas to Kilkenny and Lerdahl loams <br /> on. the slopes . All of these soils have generally high ground <br /> water elevations (6" to 3 ' ) . The Kilkenny soils have generally <br /> high (slow) percolation rates . The Marsh and Lake Beach soils � <br /> • perc fast but fail to clean nutrients or bacteria before exposure ` <br /> � to groundwater. Consequently, none of these soils is considered <br /> suitable for standard on-site sewage treatment systems by the HSWCD, <br /> � PCA, M�'WD, MHD, or City. Given suitable slopes , the Kilkenny loams <br /> will support mound type sewage treatment systems. <br />