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1 ' � 1 f <br /> mannagrasses, prairie cordgrass and mints. Meadows may be present in shallow lake basins, <br /> sloughs, farmland "sags" or may border shallow rnarshes on the landward side. <br /> Table 4 (Cowardin et al p. 28) includes within its description of Type 2 wetlands as fen and <br /> northern sedge meadow. The water regime is described as saturated (B). This description, as <br /> used by some plant ecologists and wetland scientists, is specifically limiting and at least in some <br /> instances does not suggest that reed canary grass dominated wetlands would fall into this <br /> category. <br /> Type 3—Inland Shallow Fresh Marshes <br /> Inland shallow fresh marshes (Type 3) wetlands have a soil substrate that is usually waterlogged <br /> during the growing season and at some times may be covered with as much as 6 inches or more <br /> of water. Common vegetation includes grasses, bulrushes, spikerushes, and various other marsh <br /> plants such as cattails, arrowheads, pickerelweed, and smartweeds. Common representatives in <br /> the North include reed, whitetop, rice cutgrass, carex and giant burreed. Type 3 marshes may <br /> nearly fill shallow lake basins or sloughs or may border deep marshes on the landward side. <br /> They may also occur as seep areas in agricultural fields resulting from failing drain tile systems <br /> or where sand seams are near the surface on hillside slopes. <br /> Cowardin et al (Table 4, pg 28) describes the water regime as either seasonally flooded (C) or <br /> semipermanently flooded (F). The accurate categorization of Type 3 wetlands is most critical <br /> since seasonally flooded wetlands containing reed canary grass are eligible for larger de minimus <br /> fills (up to 10,000 square feet) than cattail marshes (only 400 square feet). The difference in <br /> hydrological regimes is discussed in the next section. <br /> Type 7—Wooded Swamps <br /> Wooded swamps (Type 7) wetlands have a soil substrate that is "waterlogged to within a few <br /> inches of its surface" (Shaw and Fredine 1956, pg 22) during the growing season and often can <br /> be covered with as much as 1 foot of water. Type 7 wetlands often occur along the edges of <br /> sluggish streams, on floodplains, on flat uplands and in very shallow lake basins. In the North, <br /> trees include tamarack, arbor vitae, black spruce, balsam, red maple, and black ash. Northern <br /> evergreen swamps frequently have a thick ground cover of mosses. Deciduous swamps <br /> frequently contain beds of duckweeds, smartweeds and other herbaceous plant species. <br /> Hardwood swamps frequently are associated with Type 6, shrub swamp wetlands. <br /> Table 4 (Cowardin et al 1979, pg 28) states that Type 7 wetlands include all water regimes <br /> except permanently flooded. This description is inconsistent with the more specific description <br /> of Shaw and Fredine (1956) that describes a Type 7 wetland as having waterlogged soil to within <br /> a few inches of the surface throughout the growing season. <br /> Wooded swamps (Type 7) are frequently mischaracterized as bottomland hardwoods (Type 1L), <br /> however there are significant differences in the hydrological regimes between the two. The <br /> nature of these differences is discussed in a subsequent section. <br />