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Wetland Classification/ident/delineation-2007
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2180 Abingdon Way - 03-117-23-24-0012
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Wetland Classification/ident/delineation-2007
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Last modified
8/22/2023 4:36:09 PM
Creation date
7/26/2018 3:43:43 PM
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x Address Old
House Number
2180
Street Name
Abingdon
Street Type
Way
Address
2180 Abingdon Way
Document Type
Misc
PIN
0311723240012
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� <br /> � h k <br /> suc as wlute cedar, tamarack, and blac spruce swamps. Tlvs modifier also descnbes Type 2 <br /> , wetlands as descn�bed above and includes fens and sedge/rush dominated wetlands. <br /> , Modifier"C" <br /> Season , Flooded( eason�i) <br /> Surface water is present for extended penods especially early m the growmg season but �s absent <br /> by the ead of the season in most years. When surface water is absent, the water table is often <br /> i near the surface. Santos and Gauster (1993, pg 31) add that the water table, after flooding <br /> ceases, is very variable, extending from saturated to a water table well below the surface. This <br /> ' accurately descnbes the situaiion that frequent�y occurs within reed canary grass wetlands where <br /> there is saturation to the swface or even several inches of inundation after snow �h. In most <br /> years, by the end of May, surfa�ce water is no longer evident in, many of these basins. During <br /> ' June, the water table continues to recede unt� by August, the water table may be two or more <br /> feet below the surface. Many of these areas are used for livestock pasturing and for harvest�g <br /> ir�adow hay. Wetlands with a "C" modifier that consist predorivnantly of reed canary grass <br /> � should be categorized as either Type 1 or Type 2 depending on the length of time that water is <br /> present. This modifier is the most difficult to specifically assign to a Type 1, Type 2 or Type 3 <br /> category as it could apply to any of the three. <br /> ' ModiBer"D" <br /> �easonal Well-Urained(No comoarable Cowardin catego� <br /> , Santos and Gauster (1993, pg 31) descn`be this modifier as applyuig where surfa�e water is <br /> present for extended periods especially early in the growing season. The water table, after <br /> flooding ceases falls well below the ground surFace. This modifier would appear to apply to <br /> ' floodplains and bottomland hardwood forests (Type 1 L) as descnbed above. Modifiers "C" and <br /> "D" seem to overlap to a certain extent and could also apply to reed canary grass wetl�ds as <br /> well. <br /> � ModiBer"E" <br /> Seasonal Saturated�,No co��rable Cowardin cate�ory� <br /> ' Surface water is present for extended.periods especially early in the growing season, and remains <br /> saturated near the surface for rrwst of the growing season(Santos and Gauster 1993,pg 31). This <br /> modifier would appear to apply to fens, sedge and rush meadows, some Type 6 shrub swarn�s, <br /> 1 Type 7 Hardwood Sw� and Type 8 bogs. Sor�e re,�d canary grass wetlands might fall into <br /> this category but most seem to be dried out by early to mid-swrnner. <br /> ' ModiBer"F" <br /> Semivennanentiv Flooded(Serrri�errnanent�. <br /> Surface water persists throughout the growing season in most years. When surface water is <br /> � absent, the water table is usually at or very near the land surface (Cowardin et a1 1979, pg 22; <br /> Santos and Gauster 1993, pg 31). This modifier applies to Type 3 cattai� marshes and may also <br /> apply to some hardwood swamps such as black ash, conifer bogs and Type 6 alder shrub <br /> ' ��� <br /> , Svoboda Ecolo 'cal Resources 2180 Abin don Wa <br /> St � Y <br /> Project No.2007-056-03 Orono,Minnesota <br /> 1 <br />
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