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Wetland 4 (W4): <br />NWI Cowardin: PUBHx <br />PWI (Hydro) ID: None <br />Field Observation Circular 39: Type 3/7 <br />Field Observation Eggers and Reed: Shallow <br />Marsh/Wooded Swamp <br />Soil Mapping Unit(s): Duelm loamy <br />sand/Hubbard loamy sand <br />Wetland 4 is located in the west -central part of <br />the study area. W4 is believed to be partially <br />excavated in a historical wetland and partially <br />excavated in upland. <br />The field investigation found the site has met all <br />three wetland indicators and this portion of the <br />wetland should be considered a palustrine <br />j,q, ncP,c9 Jm 00 monmm,cn, onn�n� <br />emergent persistent seasonally <br />flooded/palustrine forested broad-leaved <br />deciduous temporarily flooded (PEM1C/PFO1A) wetland. One transect and several sample points <br />were taken to deteiniine the wetland boundary. Soils, hydrology and topography aided in <br />deteiniining the wetland boundary. <br />At the wetland pit location W4A the plant community is dominated by common Canada bluejoint, <br />giant goldenrod, riverbank grape, sandbar willow, quaking aspen, and black willow. The upland pit <br />location W4B is dominated by white sweet clover, Canada bluejoint, quaking aspen, and sandbar <br />willow. Both plant communities are considered hydrophytic. <br />Soils in the wetland pit location W4A met hydric soil indicator F3 — Depleted Matrix. Soils in the <br />upland pit location W4B did not meet any hydric soil indicators. <br />m: <br />1IIIl�'jWlywl�Wl III <br />��I��l� <br />i�� I � .I��� <br />1li <br />IIrI 'y6a"v 1,100 <br />11IIII^11iiJa <br />llllll yl� <br />11111111 <br />I➢IN'!h�' p ICI I <br />gllillklpP; ill 1 ul <br />I I II 1111111111111111111111111111111111111111111IIIIIIIIIIIIIIIIIIIII �Jl� � I�,i�,, <br />'y��i"�' mrvll �II II I�^II'i�l,i�'4 I IIiS�jl <br />111111111 <br />111111111111111111111111111111111 <br />IIIIIIIIIII IIIIIIII <br />W-I Trunseet <br />11,1111111111111111 <br />I I III I I I I I I I IJ,I,,,I, I I piI11JIUlilnl�l6 <br />uIV <br />pm <br />jl <br />1���1111111��������i,P\ll� <br />�I � uuii�llliillllllll�lll ����'luumu��r <br />Y,IIIIIIIIIII�IIII,II� J ��,,l„I, III,�,I,I,IIIIIIIIIIII�II <br />;o,;(0I!': <br />'y m lii Illlliiil IIIII <br />„�,,,,1��IIIIIIIIIIIIIIIIIIIIIIIIIII' <br />IR;IIIVII llln011l <br />Soils in the wetland pit W4A were <br />not saturated. The wetland pit <br />location met secondary hydrology <br />indicators D2 and D5. Soils in the <br />upland pit location W4B were not <br />saturated and only met secondary <br />hydrology indicator D5. <br />The deteiniining factor for this <br />delineation was the lack of hydric <br />soil and wetland hydrology <br />indicators at the upland pit <br />location. The boundaries were <br />deteiniined by following the <br />topographic break and vegetative <br />ll" break. <br />hll�llnrll 41'( <br />4 <br />11111111111111111111111111 <br />u' <br />Prepared by: Bolton & Menk, Inc. <br />Ramsey COR Wetland Analysis I OR1.128637 <br />FINDINGS <br />Page 6 <br />