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broad-leaved deciduous temporarily flooded <br />(PEMF/PFO1A) wetland. One transect and <br />several sample points were taken to deteiniine <br />the wetland boundary. Soils, hydrology and <br />topography aided in deteiniining the wetland <br />boundary. <br />At the wetland pit location W2A the plant <br />community is dominated by common black <br />willow, quaking aspen, sandbar willow, and reed <br />canary grass. The upland pit location for this <br />transect is W1B. <br />Soils in the wetland pit location W2A met <br />hydric soil indicator F6 — Redox Dark Surface. <br />Soils in the wetland pit W2A were not saturated. <br />The wetland pit location met secondary <br />hydrology indicators D2 and D5. <br />The deteiniining factor for this delineation was the lack of hydric soil and wetland hydrology <br />indicators at the upland pit location. The boundaries were deteiniined by following the topographic <br />break and vegetative break. <br />"'OH <br />I <br />Wetland 3 (W3): <br />NWI Cowardin: None <br />PWI (Hydro) ID: None <br />Field Observation Circular 39: <br />Typetet4/6 <br />Field Observation Eggers and <br />Reed: Deep Marsh/Shrub Swamp <br />Soil Mapping Unit(s): Duelm <br />loamy sand/Hubbard loamy sand <br />Wetland 3 is found in the northwest <br />part of the study area. W3 is <br />believed to be a pond excavated in <br />upland. <br />The field investigation found the <br />W3 site has met all three wetland <br />indicators and this portion of the <br />wetland should be considered a palustrine emergent semipeinianently flooded/palustrine scrub <br />shrub broad-leaved deciduous temporarily flooded (PEMF/PSS1A) wetland. No transect but several <br />sample points were taken to deteiniine the wetland boundary. Soils, hydrology and topography <br />aided in deteiniining the wetland boundary. <br />Wetland 3 is dominated by sandbar willow and cattails. The upland areas adjacent to W3 are <br />dominated by Canada goldenrod and smooth brome. <br />The deteiniining factor for this delineation was the lack of hydrophytic vegetation in the <br />surrounding upland areas. The boundaries were deteiniined by following the topographic break and <br />vegetative break. <br />IIIIIIIIIIIII,,iii °P` 'iq usu,jp111,w, <br />uuimlrl VIIIii INhllluullll i Iiii iIIIII,p;I IRP1111'I1111[1:11I°H111), 11°IIVPII151i1�l�iilliii��� <br />Ilu�ili II V <br />I, <br />ntic��1h;1! <br />IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII <br />Prepared by: Bolton & Menk, Inc. <br />Ramsey COR Wetland Analysis I OR1.128637 <br />FINDINGS <br />Page 5 <br />