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Environmentai Cansultants Wayne]acobson, P.S.S.,W.D,C., P.W.S.,A.F.S. <br /> ------------------------------------------------ <br /> 5821 Humboldt Avenue North,8rooklyn Center, MN 55430 (612) 802-6619 Cel! <br /> Email: jacobsonenv@msn.com <br /> F92 Iron-Man.ganese Masses. On flood plains, a layer 4 inches or more thick with 40 percent or <br /> more chroma of 2 or Eess and 2 percent or mare distinct or prominent redox concentrations occurring as <br /> soft iron-manganese masses with diffuse boundaries_ The layer occurs entirely within 12 inches of the <br /> soil surface. Iron-manganese masses have value and chroma of 3 or lass. Most commonly, they are <br /> black. The thickness requirement is waived if the layer is the minerai surface layer, <br /> User Notes:7hese iron-manganese masses generally are smal! (2 to 5mm in size) and have value and <br /> chroma of 3 or less. They can be dominated by manganese and therefore have a color approaching <br /> black. The low matrix chroma must be the result of wetness and not be a weathering or parent material <br /> feature. Iron-manganese masses should not be confused with the larger and redder iron nodules <br /> associated with plinthite or with concretions that have sharp boundaries. This indicator occurs on ffood <br /> plains along rivers, such as the Apalachicola, Congaree, Mobile, Savannah, and Tennessee Rivers. ', <br /> HvdroJoqv � <br /> The presence of current we#iand hydrology was deterrnined through direct observation of free water in the <br /> excavated soil pit, saturated soil conditions or soil redoximorphic features. However, the effect of on-or <br /> off-site hydrologic alterations may not always fuily be accounted for when routine delineation methods are <br /> used. <br /> In the Midwest Region, hydrology indicators are in faur groups: <br /> A)indicators based on the direct observation of surface water or groundwater during a site visit <br /> lndicator A1: Surtace water <br /> Category: Primary <br /> General Description: This indicator consists of the direct, visual observation of sunrace water(flooding or <br /> ponding}during a site visit. <br /> Indicator A2: High water table <br /> Category: Primary <br /> General Description: This indicator consists of the direct, visual observation of the water table 12 in (30 <br /> cm}or less below the surface in a soil pit, auger hole, or shallow monitoring well. This indicator includes <br /> water tabfes derived from perched water, throughflow, and discharging groundwater(e.g., in seeps) that <br /> may be moving laterally near the soil surface. <br /> Indicator A3: Saturation <br /> Category: Primary <br /> Generat Description: Visual observation of saturated soil conditions92 in. (30cm)or less from soil surface <br /> , as indicated by water glistening on the surfaces and brofcen interior faces of soil samples removed from <br /> ttie pit or auger hole. This indicator must be associated with an existing water table focated immediately <br /> below the saturated zone; however, this requirement is waived under episaturated conditions if there is a <br /> restrictive soil layer or bedrock within 12 in. (30 cm}of the surface. <br /> 8) indicators of evidence that the site is subject to flooding or panding <br /> Indicator B1: Water marks <br /> Category; Primary <br /> General Description: water marks are discolorations or stains on the bark of woody vegetation, rocks, <br /> bridge supports, buildings, fences,or other fixed objects as a result of inundation. <br /> Wetland Delineation-Mitigation-Permitting-Monitoring-Banking-Functional Analysis-T& E Surveys g <br /> Phase I Environmental Assessments-EAW's-Soil ID-Soil Analysis&pelineation-Environmental Referrafs <br /> Pond &Lake Weed Control &Fish Stocking-7ree Surveys-Nakural Resource Management Plans <br />