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Draft North & East Metro Groundwater Management Area Plan 2-1 <br /> 2. Description of the Boundary and the GWMA <br /> A geographic area was defined within which to manage groundwater resources.The boundary for this <br /> GWMA was selected by using a combination of physical,governmental, and planning elements. <br /> Establishing a boundary allows us to identify and analyze factors that affect long term water use, and to <br /> identify specific actions that reduce the risk of unsustainable groundwater use. <br /> Elements considered in selecting the boundary of the GWMA included the following: <br /> • Hydrogeology <br /> • Water use <br /> • Water dependent natural resources <br /> • Water quality <br /> • Jurisdictions, governance and planning <br /> The boundary selected for the North & East Metro GWMA includes all of Washington and Ramsey <br /> counties, 10 cities in southeastern Anoka County, and the portion of Hennepin County east of the <br /> Mississippi River(Figure 2-1). Vertically, the boundary includes all parts of the groundwater system <br /> above the Eau Claire geologic formation.A more detailed description of the elements listed above is <br /> given in the documents: Draft Working Boundary N& E Metro GWMA and Updated Draft Working <br /> Boundary N& E Metro GWMA. Section 2 of this Plan provides summary information on the elements <br /> that were used to select the boundary for the North & East Metro GWMA. <br /> Hydrogeology <br /> Hydrogeology defines the natural conditions and boundaries of the groundwater system.The boundary <br /> includes the following: <br /> • The horizontal extent of the Prairie du Chien—Jordan aquifer between the hydrologic boundaries <br /> formed by the Mississippi and St. Croix rivers, except for localized outliers of these bedrock <br /> formations(Figure 2-2) <br /> • The hydrogeological transition area in southeastern Anoka County and Forest Lake in <br /> Washington County adjacent to the margin of the Prairie du Chien—Jordan aquifer <br /> • All aquifers above the Eau Claire Formation confining unit (Figure 2-3). The Mt. Simon aquifer <br /> (located below the Eau Claire Formation) is not included because it is hydrologically separated <br /> from the shallower aquifers within the area.Appropriations from the Mt. Simon are also <br /> restricted by statute in the seven county Twin Cities Metropolitan Area. <br /> Topographic watershed boundaries were reviewed. The watersheds are integral to groundwater health <br /> but generally do not match the hydrogeologic boundaries to the regional groundwater system. <br /> P29 <br />