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�LAND DE�NITION <br /> According to the 1987 U.S. Army Corps of Engineers "Wetlands Delineation Manual" (1987 <br /> Manual; the document used by all delineators to define wetlands) a wetland is "Those areas that <br /> are inundated or saturated by surface or ground water at a frequency and duration sufficient to <br /> support, and that under normal circumstances do support, a prevalence of vegetation typically <br /> adapted for life in saturated soil conditions." The Minnesota State Wetland Conservation Act <br /> Rules, Chapter 8420, further clarifies that "...wetlands must: (1) have a predominance of hydric <br /> soils; (2) be inundated or saturated by surface water or groundwater at a frequency and duration <br /> sufficient to support a prevalence of hydrophytic vegetation typically adapted for life in saturated <br /> soil conditions; and (3) under normal circumstances, support a prevalence of hydrophytic <br /> vegetation." The 1987 U.S. Army Corps of Engineers Manual in Part II, item 24. states that, <br /> "The interaction of hydrology, vegetation, and soil results in the development of characteristics <br /> unique to wetlands. Therefore, the following technical guidelines for wetlands are based on the <br /> ' three parameters, and diagnostic environmental characteristics used in applying the technical <br /> guideline are represented by various indicators of these parameters." It is this premise by which <br /> SER ecologists has, in their professional judgment, delineated the wetlands on the subject parcel <br /> described in this report. <br /> Wetland Hydrology <br /> The most important wetland criterion is hydrology. The presence and persistence of water <br /> influences the vegetation types and changes soil morphology. Hydrology may be observed as <br /> standing water(inundation), or may be observed as freestanding water within the soil pit or auger <br /> hole (saturation) usually within the upper 12 inches. This is what would be considered primary <br /> hydrology indicators. Only one primary indicator is necessary to make the determination that <br /> wetland hydrology indeed exists. The 1987 Corps Manual also has a range of hydrologic zones <br /> established based on period of inundation or saturation. These zones and the periods of <br /> inundation or saturation for each can be observed in Table 1 below. <br /> ' Exce ted from the 1987 Manual,Hydrolo ic Zones—Nontidal Areas <br /> Zone Name Duration Comments Wetland or Not <br /> I Permanently Inundated 100% Inundation>6.6 ft. mean Not(Aquatic Habitat Zone,or Deep Water <br /> water de th Habitat) <br /> Semipermanently To Nearly �75 Inundation defined as <br /> II Permanently[nundated Or <100% �6.6 feet mean water Wetland <br /> Saturated de th <br /> III Regularly Inundated Or >25-75% Wetland <br /> Saturated <br /> IV Seasonally Inundated Or <12.5- Wetland <br /> Saturated 25% <br /> Irregularly Inundated or o Many areas having these Wetland(if hydrophytic veg.and hydric <br /> V Saturated �5-12.5/o hydrologic characteristics soils also present <br /> are not wetlands <br /> [ntermittently Or Never o �eas with these <br /> VI <5/o hydrologic characteristics Not <br /> Inundated Or Saturated are not wetlands <br /> A-1 <br />