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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 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 indicator A3 (Saturation) as well as secondary hydrology <br /> indicators C2 (Dry-Season Water Table) and D2 (Geomorphic Position). At sample points 1-1 <br /> UP and 1-2, UP no hydrology indicators were present as the samples were located upslope, <br /> approximately 1-2 feet higher in elevation than 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, fresh <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 PFO1C, Type 1L, <br /> floodplain forest. The wetland vegetation was dominated by reed canary grass (Phalaris <br /> arundinacea FACW) in the herb stratum for all sample points and green ash (Fraxinus <br /> pennsylvanica FACV� in the shrub stratum in sample point 2-3 WET. The transition to upland <br /> can be marked 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 /> canadensis FACU)become prevalent. <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 depletions. The web soil survey indicates the soil series as <br /> Glencoe loam. The soils at sample point 2-2 WET consisted of clay for 30 inches of depth with <br /> concentrations 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 Houghton soils. T'he soils at <br /> sample point 2-3 WET consisted of clay 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 all three wetland <br /> sample locations. <br /> The soils at sample point 2-1 UP consisted of clay for 24 inches of depth with concentrations at <br /> 12-24 inches. The web soil survey indicates the soil series as Lester loam. The soils at sample <br /> point 2-2 UP consisted of clay for 36 inches of depth with concentrations present below 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 for 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 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 of primary indicator A3 (Saturation) at sample point 2-1 WET. At sample points 2- <br /> 1 UP, 2-2, UP and 2-3 UP no hydrology indicators were present as they were located upslope <br /> approximately two feet higher in elevation than the three wetland samples. <br /> Svoboda Ecological Resources 300&350 Stubbs Bay Road <br /> Project Number: 2014-037-03 4 Orono <br />