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_ The Soil Survey of Hennepin County indicates five individu�! soil types on the subjeCt pro�erty <br /> (Figure 3}. These individual soil types include: Kilkenny loam {KkB and C), Lester clay loam <br /> (LsD2), Hamel loam (Ha), Le Sueur loam (LtB) and Palms peaty muck (Pm}. See Appendix C � <br /> , for a description of the soil series for each of these soi! types. Of these soil types, the Hamel loam <br /> (Ha) and the Palms peaty muck (Prrt) are classified as hydric soils (Hydric Soils of the United <br /> States). The DNR Pub[ic Waters Map of Hennepin County illustrates no public waters on the <br /> - . subject property (Figure 4). <br /> SER personnel examined the subject property foc areas meeting jurisdictionat wetland criteria <br /> � during the site visit and delineated two areas as being jurisdictional wetfand. Detailed vegetation, <br /> soils, and hydrology data for the wetEand are provided in the data sheets of <br /> Appendix A. <br /> � Basin 1 is located in the in the southern portion of the western property (Figure 5). SER <br /> ! delineated the boundary of Basin 1 as a palustrine (P-) type wetland ex[�ibiting emergent (-EM-) <br /> vegetation with a seasonally flooded(-C-) moisture regime that is ditched (-d) or a Type 3 <br /> . (PEMCd) wetland. Basin 1 is 40,404 square feet(0.928 acres) in size. <br /> The wetland boundary was based on the transition in elevation from wetland to upland. <br /> � Normally a vegetation dominance wauid be used to identify the boundary but a dominance of <br /> . Reed Canary Grass (Phalaris arundinacea, FACW+) exists in the upland as well as the wetland. <br /> SoiIs and hydrology were also used as a way to further justify the placement of the boundary at <br /> various unmazked Iocations azound the basin as well as the marked transects where vegetation, <br /> hydrology, and soils data was coIlected and recorded. <br /> � SER used 23 lath to delineate the wetland boundary of Basin 1. � <br /> Basin 2 is located in the soutl�-central partion of the eastern property(Figure 5). SER delineated <br /> the boundary of Basin 1 as a palustrine(P-) type wetland exhibiting emergent {-EM-) vegetation <br /> ,.,, with a seasonally flooded{-C-) moisture regime that is ditched (-d) or a Type 3 (PEMCd) <br /> wetland. Basin 2 is 10,339 sc�uare feet(0.237 acres) in size <br /> The wetland boundary was based on the transition in elevation from wetland to upland.Normally <br /> a vegetation dominance would be used to identify the boundary but a dominance of Reed Canary <br /> Grass (Phalaris arundinacea,FACW+)exists in the upland as well as the wetland. Soils and <br /> hydrology were also used as a way to further justify the placement of the boundary at various <br /> unmarked locations azound the basin as well as the marked transects where vegetation, <br /> hydrology, and soils data was co3lected and recorded. <br /> SER used 171ath to delineate the wetland boundary of B'asin 2. <br /> Photographs 1 through 4 (Photo Log) depicts Basins 1 and 2 at the time of the site visit. <br />