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with concentrations and depletions between 14-20 inches. The web soil survey indicates the soil <br /> series as Hamel-Glencoe. Hydric indicator Al2 (Thick Dark Surface} was present at sample <br /> locations 1-1 UP. <br /> Wetland hydrology was present at sample point 1-1 VVET as signified by primary indicator A3 <br /> (Saturation) as well as secondary hydrology indicators C2 (Dry-Season Water Table), D2 <br /> (Geomorphic Position) ansi DS (FAC-Neutral Test). Wetland hydrology was present at sample <br /> point 1-2 WE'T as signified by primary indicator A3 (Saturation) as well as secondary hydrology <br /> indicators C2 {Dry-Season Water Table) and D2 (Geomorphic Posirion}. At sample points 1-1 <br /> UP and 1-2, UP no hydrology indicators were presern as the samples were located upslope, <br /> approxunately 1-2 feet higher in elevation than the twa wetland samples. <br /> Basin 2 <br /> The majarity of the second wetland basin on this parcel is classified as a PEMC, Type 2, freah <br /> (wet) meadow wetland located north, east azid south of the residence driveway. East af sample <br /> transects 2-2 and 2-3 there is a portion of the wetland basin classified as PFO1C, Type 1L, <br /> floodplain forest. The wetland vegetation was dominated by reed canary grass (Phalaris <br /> arundinacea FAC`U� in the herb stratum for all sample points and green ash {Fraxinus <br /> pennsylvanica FACV� in the ahrub stratum in sample point 2-3 WET. The transition to u}�land <br /> can be marked by the change in vegetation community. The further upslope the mrnre upland <br /> species, such as Kentucky biuegrass {Poa pratensis FAC) and Canada goldenrod (Solidago <br /> canadensis FAC[�become prevaient. <br /> The soils at sample point 2-1 WET consisted of clay for 22 inches of depth where it changes to a <br /> sandy clay with concentrations and depletians. The web eoil survey indicates the soii series as <br /> Glencoe loam. The soils at sarnple point 2-2 WET consisted of clay for 3Q inches of depth with <br /> concentrations present belaw 12 inches and a depleted matrix present below 20 inches. The web <br /> soil survey indicates the soil series as Muskego, Blue Earth, and Houghton soils. The soils at <br /> sample point 2-3 WET consisted of clay for 28 inches of depth where it changes to a sandy ciay <br /> with a depleted matriac and concentrations. The web soil survey indicates the soil series as <br /> Cordova loazn. Hydrie inclicator Al2 (Thick Dark Surface) was present at all three wetland <br /> sample Iocations. <br /> The soils at sample point 2-1 UP consisted of clay for 24 inches of depth with coneentrations at <br /> 12-24 inches. The web soil suuvey indicates the soil series as Lester loam. The soils at sample <br /> point 2-2 UP coxisisted of clay for 36 inches of depth with concentrations present below 12 <br /> inches and a depleted matrix bel.ow 30 inches. The web soil survey indicates the soil series as <br /> LeSueur loam. The soils at sample point 2-3 UP consisted of clay for 38 inches af depth with a <br /> depleted matrix with concentrations &om 30-3$ inches. The web soil survey indicates the soil <br /> series as Cordova loam. Hydric indicator Al2 (Thick Dark Surface) was present at all three <br /> upland sample locations. <br /> Wetland hydrology was present at sample points 2-1 WET, 2-2, WET and 2-3 WET as signified <br /> by secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC-Neutral Test} with <br /> the addition af prunary indicator A3 (Saturation} at sample point 2-1 WET. At sarnple points 2- <br /> 1 UP, 2-2, UP and 2-3 UP no hydrology indicators were present as they were Iocated upslope <br /> approximately two feet higher in elevation than the three wetland samples. <br /> Svoboda Ecolo�cal Resources 300&350 5tubbs Bay Road <br /> Project Number:2014037-03 q Omno <br />