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• Basin ID: Basin B <br />Page 4 of 4 <br />Disturbance Factors <br />Apparently a staging area for access to the Island. Fill/disturbance is evident along the upland access trail and as an apparent <br />pad in the transition to the undisturbed wetland. The surface Is hummocky with obvious peat/mineral fill piles. Extreme <br />evidence of subsidence in the area of the transition from disturbed upland to wetland. Occasional large voids (holes several <br />inches in diameter) were observed when augering soli. Boxelder in obvious upland positions have exposed roots several <br />inches above the current soil surface probably exposed by subsidence /consolidation /oxidation. Subsoils powdery-dry when <br />examined. <br />Floristic Features <br />Disturbed area dominated by reed canary grass/stinging nettle. Reed camary grass/nettle area delineated as wetland. <br />Transition zone contains large quantities of bucicthon both in the shrub and herb layers. <br />Soil Factors <br />Entire area near the access is probably filled /disturbed; however, some profiles looked native, others consisted of obvious fill. <br />Soils were generally transitional variants between upland hayden /Dundas/Markey that have been scalped /filled. Much <br />evidence of subsidence, including elevated tree roots in areas that have no evidence of inundation, and observed cavaties in <br />the subsoils. Anomalous redox concentrations indicative of a water table at approximately 30 -40 inches were observed deep <br />in one soil profile near the wetland boundary. <br />Hydrology Factors <br />No water to 40 inches In all profiles examined. <br />Other Comments <br />Portions of the staging area (Basin B) that were delineated as wetland may be filled to the extent that wetland hydrology is <br />missing. <br />Copyright Peterson Environmental Consulting, Inc. <br />