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with concenirations and depletions between 14-20 inches. The web soil survey indicates the soil <br /> series as Hamel-Glencfle. Hydric indicator Al2 (Thick Dark Surface) was present at saYnple <br /> locatians 1-1 UP, <br /> Wetland hydrology was present at san�le point 1-1 WET as signified by primary indicator A3 <br /> (Saturation} as well as secondary hydrology indicators C2 (Dry-Season Water Table), D2 <br /> {Geomorphic Position) and DS (FAC-Neutral Test). Wetland hydrology was present at sample <br /> point 1-2 WET as signified by primary indicaxor A3 (Saturation) as well as secondary hydrology <br /> indicators C2 {Dry-Season Water Table) and D2 (Geomorphic Position). At sample points 1-1 <br /> U�' and 1-2, UP no hydrology in,d.icators were present as the samples were located upslope, <br /> approximately 1-2 feet higher in elevarion thau the two wetland samples. <br /> Basin 2 <br /> The majority of the second wetland basin on this parcel is classified as a PEMC, Type 2, fi�esh <br /> (wet) meadow wetland located north, east and south of the residence driveway. East of sample <br /> transects 2-2 and 2-3 there is a portion of the wetland basin classified as PFO 1 C, Type 1 L, <br /> floodplain forest. The wetland vegetation was dominated by rced canary grass (Phalari,s <br /> arundinacea FACV� in the herb stratum for a.11 sample points and green ash (Fraxfnus <br /> pennsylvanica FACV� in the shrub stratum in sample point 2-3 WET. The transition to upland <br /> can be m�rked by the change in vegetation community. The further upslope the more upland <br /> species, such as Kentucky bluegrass (Poa pratensis FAC) and Canada goldenrod (Solidago <br /> canadensi�FACLn become prevalemt. <br /> The soils at sample point 2-1 WET consisted af clay for 22 inches of depth where it changes to a <br /> sandy clay with concenntrations and depletions. The web soil survey indicates the soil series as <br /> Glencoe loam. The soils at sarnple point 2-2 WET consisted of clay for 30 inches of depth with <br /> concenirations present below 12 inches and a depleted matrix present below 20 inches. The web <br /> soil survey indicates the soil series as Muskego, Blue Earth, and Haughton soils. The soils at <br /> sample point 2-3 WET consisted of ciay for 28 inches of depth where it changes to a sandy clay <br /> with a depleted matrix and concentrations. The web soil survey indicates the soil series as <br /> Cordova loam. Hydric indicator Al2 (Thick Dark Surface) was present at au three we�land <br /> sampie locations. <br /> The soils at sample point 2-1 UP consisted of clay for 24 inches of depth with concen,trations at <br /> 12-24 inches. The web soil survey indicates the soil series as Lester loam. The soils at saznple <br /> point 2-2 UP consisted of clay for 36 inches of degth with concentrations present beiow 12 <br /> inches and a depleted matrix below 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 far 38 inches of depth with a <br /> depleted matrix with concentrations from 30-38 inches. The web soil survey indicates the soil <br /> series as Cordova loam. Hydric indicator Al2 {Thick Aar}� Surface) was present at all three <br /> upland sample locations. <br /> Wetland hydralogy was preaent at sample points Z-1 WET, 2-2, WET and 2-3 WET as signified <br /> by secondary hydrology indicators D2 (Geomorphic Position) and DS {FAC-Neutral Test} wi� <br /> the addition of primary indicator A3 (Saturation) at sample point 2-1 WET. At sample points 2- <br /> 1 L�', 2-2, UP and 2-3 UP no hydrology indicators were present as they were located upslope <br /> approximately two feet higher in elevation th�n the three wetland samples. <br /> Svoboda Ecological Resourcea 300&350 Stubbs Bay Rosd <br /> Project Number: 2014-037-03 4 Omno <br />