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1987 Wetland Delineation Manual - The Wetlands Regulation Center

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<strong>Wetland</strong> Delination <strong>Manual</strong>, <strong>1987</strong> 69<br />

bring nonwetland areas having wetzand indicators of two, but not all three, parameters into<br />

Section 404 jurisdiction.<br />

a. <strong>Wetland</strong>s on drumlins. Slope wetlands occur in glaciated areas Tn-which thin soils cover<br />

relatively impermeable glacial till or in which layers of glacial till have different hydraulic<br />

conditions that produce a broad zone of ground-water seepage. Such areas are seldom, if ever,<br />

flooded, but downslope groundwater movement keeps the soils saturated for a sufficient<br />

portion of the growing season to produce anaerobic and reducing soil conditions. This fosters<br />

development of hydric soil characteristics and selects for hydrophytic vegetation. Indicators of<br />

wetland hydrology may be lacking during the drier portion of the growing season.<br />

b. Seasonal wetlands. In many regions (especially in western states), depression areas occur<br />

that have wetland indicators of all three parameters during the wetter portion of the growing<br />

season, but normally lack wetland indicators of hydrology and/or vegetation during the drier<br />

portion of the growing season. Obligate hydrophytes and facultative wetland plant species<br />

(Appendix C, Section 1 or 2) normally are dominant during the wetter portion of the growing<br />

season, while upland species (annuals) may be dominant during the drier portion of the<br />

growing season. <strong>The</strong>se areas may be inundated during the wetter portion of the growing<br />

season, but wetland hydrology indicators may be totally lacking during the drier portion of the<br />

growing season. It is important to establish that an area truly is a water body. Water in a<br />

depression normally must be sufficiently persistent to exhibit an ordinary high-water mark or<br />

the presence of wetland characteristics before it can be considered as a water body potentially<br />

subject to Clean Water Act jurisdiction. <strong>The</strong> determination that an area exhibits wetland<br />

characteristics for a sufficient portion of the growing season to qualify as a wetland under the<br />

Clean Water Act must be made on a case-by-case basis. Such determinations should consider<br />

the respective length of time that the area exhibits upland and wetland characteristics, and the<br />

manner in which the area fits into the overall ecological system as a wetland. Evidence<br />

concerning the persistence of an area's wetness can be obtained from its history, vegetation,<br />

soil, drainage characteristics, uses to which it has been subjected, and weather or hydrologic<br />

records.<br />

c. Prairie potholes. Prairie potholes normally occur as shallow depressions in glaciated<br />

portions of the north-central United States. Many are landlocked, while others have a drainage<br />

outlet to streams or other potholes. Most have standing water for much of the growing season<br />

in years of normal or above normal precipitation, but are neither inundated nor have saturated<br />

soils during most of the growing season in years of below normal precipitation. During dry<br />

years, potholes often become incorporated into farming plans, and are either planted to row<br />

crops (e.g. soybeans) or are mowed as part of a haying operation. When this occurs, wetland<br />

indicators of one or more parameters may be lacking. For example, tillage would eliminate<br />

any onsite hydrologic indicator, and would make detection of soil and vegetation indicators<br />

much more difficult.<br />

d. Vegetated flats. In both coastal and interior areas throughout the Nation, vegetated flats are<br />

often dominated by annual species that are categorized as OBL. Application of procedures<br />

25 February 1997 Environmental Techncal Services Co. 834 Castle Ridge Rd Austin, Texas 78746

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