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Botanical Garden, 1991 ). Indicator status of plant species was taken from the 2012 National <br />Wetland Plant List (Lichvar, R.W. and Kartesz, J.T. 2009. North American Digital Flora: <br />National Wetland Plant List, version 2.4.0 (https://wetland_plants.usace .army.mil). U.S. Arm y <br />Corps of Engineers, Engineer Research and Development Center, Cold Regions Research and <br />Engineering Laboratory, Hanover, NH, and BONAP, Chapel Hill , NC.) <br />III.RESULTS <br />Review of Soils, NWI, and DNR Information <br />The National Wetland Inventory Map (NW/) (Mound Quadrangle, U.S. Fish & Wildlife Service <br />1989) showed one PUBG:x/PEMA wetland within the site boundaries (Figure 3). <br />The Soil Survey of Hennepin County, Minnesota <br />(http://soils.usda.gov/survey/geography/ssurgo/) showed the following soil types within or near <br />site boundaries (Figure 4). Partially hydric means that at least one component of the map unit is <br />rated as hydric . <br />SMU Map Unit Name Hvdric? <br />L22E Lester loam, morainic, 18 to 25 percent slopes Partially hvdric <br />L23A Cordova loam, 0 to 2 percent slopes Partially hydric <br />L36A Hamel, overwash-Hamel complex, 1 to 4 percent slopes Partially hydric <br />L40B Angus-Kilkenny complex, 2 to 6 percent slopes Partially hydric <br />L41C2 Lester-Kilkenny complex, 6 to I 2 pe rcent slopes, eroded Partially hydric <br />L41E Lester-Kilkenny complex, 18 to 25 percent slopes Partially hydric <br />The DNR Protected Waters Map, Hennepin County (http://deli.dnr.state.mn.us/) did not show <br />any DNR Protected Waters, Waterways, or Wetlands within or near site boundaries (Figure 5). <br />Wetland Determinations and Delineations <br />Potential wetlands were evaluated in greater detail during field observations on October 1, 2012. <br />One wetland was identified and delineated on the subject s ite (Figure 2). Corresponding data <br />forms are included in Appendix A. The following description of the wetland and adjacent <br />upland reflects conditions observed at the time of the field visit. At that time, herbaceous <br />vegetation was actively growing and temperatures were typical of the season. Wetland <br />hydrology was assumed to be drier than typica l for that date based on below normal precipitatio n <br />amounts in for the preceding 30 days (Appendix B). The survey of the wetland boundary is <br />presented in Appendix C. <br />Wetland 1 was a Type 4 (PUBG:x/PEMA) excavated, open water and fresh (wet) meadow <br />wetland complex. The PUBGx portion of the wetland was un-vegetated and dry. The center of <br />the basin was an upland knoll dominated by a canopy of boxelder. For the purposes of this <br />delineation it was included within the wetland boundary. Fresh (wet) meadow was dominated by <br />reed canary grass with lesse r amounts of giant goldenrod and Canada thistle. Other non- <br />3
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