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V CJ` <br /> Alternative 4: N Pro'ect <br /> Under this alternative, groundwater levels would be expected to remain well below the <br /> existing ground surface and would not cause inundation of ground-surface or impacts to F <br /> crop productivity. <br /> Mitigation-Measure 4..2=6a=-Altematives-1I2 and 3) <br /> The maximum depth of mining shall be a minimum of six feet above the seasonal <br /> high water level. As a basis for initial and ongoing mining depths, the proponent shall <br /> submit annually the results of quarterly monitoring reports to the Department Services, <br /> Division which document the groundwater elevations for a min►murrit_o.fen was <br /> supplylwells-around-the-general Perimeferof-t pem�itted"mining area. In the event <br /> _. - - <br /> that the proponent is unable to obtain or retain measurements from at least ten <br /> existing water wells, the proponent shall procure new wells for monitoring purposes <br /> at locations acceptable to the Development Services Division. The proponent shall <br /> provide a verifiable bench mark at each well site that can be referenced for <br /> compliance monitoring. Based on the water depth monitoring reports, Development <br /> Services Division may recalculate the expected high groundwater elevation, thereby <br /> adjusting the maximum depth of mining. <br /> Level of Significance After Mitigation: <br /> 9 9 <br /> Following implementation of Mitigation Measure 4.2-6a, the impact of fluctuating <br /> groundwater levels would be reduced to a less-than-significant level. i <br /> All Quar1y_Excavation Alternatives (1, 2. and 3l <br /> Impact 4.2-7 <br /> sDeyeilopment ofj.PerchedGroundwater <br /> Alternatives 1, 2, and 3 propose the construction and operation of processing wastewater <br /> basins. The initial basin would be constructed within the Phase IV mining area.. The depth <br /> of the basin is not presented in the reclamation plan. The basin would be unlined allowing <br /> percolation of the processing water into the underlying sand and gravel deposits. Complex <br /> stratigraphy in the area of the initial basin indicate that fine-grained layers of sediment <br /> could impede downward migration of the percolating water and possible development of <br /> perched groundwater. The perched groundwater could potentially be discharged along the <br /> excavation slopes, possibly resulting in erosion or failure of the slopes. In addition, <br /> perched groundwater could flow under the Delta Mendota Canal, located 800 feet east of <br /> the proposed basin under Alternatives 1 and 2 or the California Aqueduct (under <br /> Alternative 3 only). If significant pore water pressure develops, the structural integrity of <br /> the canals could be compromised. This is a significant impact. <br /> Draft Environmental Impact Report 4-22 ER-96-3 <br />