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and discharges into a wetland on the south side of the DNR trail (DNR #82-373W). Water from <br />the wetland flows in a ditch to Lake DeMontreville, <br />The 100-year flood level of Long Lake was lowered about 4 feet to Elevation 943.2 as a <br />result of the new outlet construction. One home on the lake is still in the flood plain. The first <br />floor elevation of this home is at approximately 942.8; the basement is at an even lower <br />elevation. The owner of the home chose not to participate in VBWD's residual floodproofing <br />program, so the home is still in the floodplain. Another lakeshore home has a low walkout <br />elevation at 943.3, just above the 100-year flood elevation. It is unlikely that VBWD will lower <br />the 100-year flood elevation to prevent flooding of the lowest home on the lake. Without <br />creating additional storage elsewhere, the only way the flood elevation could be lowered is by <br />lowering the outlet elevation. DNR regulations will not allow lowering of the Long Lake outlet <br />beyond that which is specified in VBWD's DNR-approved operating plan. <br />4.2.5.3 VBWD Water Quantity Management Goals <br />VBWD computed the 100-year flood elevation of Long Lake assuming ultimate <br />development in the watershed and the construction of new restricted outlets for Echo Lake and <br />Weber Pond, in the City of Mahtomedi. Based on these upstream alterations, the Long Lake <br />flood level will not increase as a result of development in the upstream watershed. However, <br />it is important that the City of Mahtomedi maintain the culverts under Long Lake Road to <br />ensure that the flood storage in the wetland north of Long Lake Road is available for storm <br />events. <br />If ravine erosion is shown to be a problem on the west shore of Long Lake, VBWD will <br />determine if remedial measures should be taken to correct and prevent erosion problems, Such <br />remedial measures could include ravine restoration, pipe installation and/or additional <br />upstream stormwater detention. <br />VBWD will continue to monitor Long Lake water levels monthly and supply the <br />information to the DNR. <br />4.2.5.4 Water Oualitv and DNR Data <br />A 1989 DNR fisheries survey of the north Long Lake basin showed higher than local <br />average northern pike, panfish and bullhead catches. A 1982 DNR fisheries survey of the south <br />Long Lake basin found average numbers of northern pike, panfish and bullheads. Because of <br />the steep shores, emergent vegetation covers only a small portion of the lake surface. The 1989 <br />DNR fisheries survey also noted water plantain and softstem bulrush on the sand delta on the <br />southwest side of the north Long Lake basin. Curlyleaf pondweed was the abundant aquatic <br />vegetation, especially in sheltered areas on the southwest and north sides of the lake. MDNR <br />has no plans to stock the lake with fish since there is no public access. Access can be gained <br />to the north basin from Long Lake Road on the north end of the lake, although this has become <br />more difficult since the road was raised. It is also possible to access the south basin from the <br />T.H. 36 south service road (Viking Drive). <br />VBWD collected water quality samples in 1971, 1972, 1975, 1979, 1984, 1987, 1990 and <br />1993. The samples were collected from the north Long Lake basin only, except for one year <br />when samples were collected from both the south and north basins. The lake is thermally <br />stratified to a depth of 10to 20 feet in summer and the cold lower waters (hypolimnion) show <br />almost no oxygen present. Total phosphorus concentrations are higher in the hypolimnion, <br />indicating that internal loading may be a significant factor in determining the water quality of <br />the lake. Summer total phosphorus concentrations have averaged 0.050 mg/L. Residents <br />23\82\045\SEC4.RPT\KMH 13 DRAFT: June 23, 1994 <br />