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02-21-23-WS
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1700 Highway 96 Site <br />4.3 Other Areas <br />Wetland Delineation Report <br />Four ephemeral tributaries were present on the site (See Figure 2), which were all resulting from <br />point discharge of stormwater. The ephemeral tributaries present all exhibited an eroded bed and <br />bank. Tributaries 1-4 were flowing sluggishly at the time of the field visit, but would likely be <br />dry during the later portions of the growing season except for immediately after rainfall events. <br />Given the presence of a defined bed and bank, these features were determined to be non -wetland <br />tributaries. The locations of observed culverts and drain tile inlets and outlets are shown on <br />Figure 2. <br />Clay drain tile was observed south of Wetland 5 that appeared to be failing based upon adjacent <br />erosion (between Wetland 5 and the origin of Tributary 2), however flowing water was only <br />observed above and below this section of tile. Given the presence of a defined bed and bank and <br />the presence of adjacent culverts discharging stormwater these areas were not delineated as <br />wetlands. Reference photos have been included as Appendix D. <br />A graded swale dominated by reed canary grass was present on the western portion of the site <br />draining from a culvert outlet into Wetland 9. The graded swale was dominated by reed canary <br />grass, with adjacent steep slopes dominated by reed canary grass, smooth brome and common <br />milkweed. This area was not delineated as a wetland because it consisted of a graded linear <br />channel that was apparently created to convey stormwater. Reference photos have been included <br />as Appendix D. <br />Sample Point A was taken on the central portion of the site within a topographic depression <br />dominated by green ash trees, gray dogwood, red -osier dogwood, Kentucky bluegrass, reed <br />canary grass, Canada goldenrod and ground ivy. This area was not shown as a wetland on the <br />NWI map, and was located within an area mapped as Hayden fine sandy loam (Predominantly <br />Non-Hydric) on the soil survey. The soils in this area did not meet a hydric soil indicator, <br />therefore this area was determined to be upland. <br />Sample Point B was taken on the northeast portion of the site within a topographic depression <br />dominated by reed canary grass and common burdock. This area was not shown as a wetland on <br />the NWI map, and was located within an area mapped as Hayden fine sandy loam <br />(Predominantly Non-Hydric) on the soil survey. This area did not contain a hydrophytic plant <br />community and the soils did not meet a hydric soil indicator, therefore this area was determined <br />to be upland. <br />No other depressional areas with hydrophytic vegetation or wetland hydrology were observed on <br />the site. No other areas were shown as wetland on the NWI map, and no other areas were <br />mapped with hydric soil on the soil survey. <br />4.4 Request for Wetland Boundary and Jurisdictional Determination <br />Appendix A of this report includes a Joint Application Form for Activities Affecting Water <br />Resources in Minnesota, which is submitted in request for: (1) a wetland boundary and type <br />determination under the Minnesota Wetland Conservation Act (WCA), and (2) delineation <br />
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