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6.Other Statutory Considerations _ <br /> Geology, Soils, And Seismicity <br /> Impact 6.6: The slope instability hazards would remain specific to the proposed RMC <br /> project site and be localized with the active mining area and therefore would not contribute <br /> to a region-wide cumulative slope instability condition.This would be a less-than-significant <br /> impact. <br /> The Proposed would result in potential geologic hazard impacts related to slope instability and <br /> seismic hazards. Similar to the other proposed and existing mining projects,the slope instability <br /> hazards would remain specific to the proposed RMC project site and be localized with the active <br /> mining area and therefore would not contribute to a region-wide cumulative slope instability <br /> condition, if one did exist. The project would attract additional workers to the mine and could <br /> place additional people in harms way during an earthquake. The project,therefore, could be <br /> responsible for contributing to a cumulative seismic risk impact as other proposed and existing <br /> projects in the region attract workers into the area. However, the number of workers added to a <br /> region from the proposed RMC project and other mining projects in this undeveloped area is <br /> negligible when considering the overall population that would be exposed to potential harm from <br /> a large regional earthquake. Because of this,the project's contribution is not cumulatively <br /> considerable and the cumulative impact is less than significant. _ <br /> Mitigation: No mitigation is required. _ <br /> Hydrology and Water Quality <br /> Impact 6.7: With mitigation,the project would not contribute to cumulative,regional <br /> adverse impacts on the lower Tulare Formation aquifer. Cumulative impacts would be <br /> potentially significant. <br /> Groundwater Consumption <br /> The cumulative impact analysis for hydrology and water quality considers the region surrounding <br /> the project site(including the city of Tracy)that currently or in the future,may extract <br /> groundwater from the extensive confined groundwater aquifer in the lower Tulare Formation(see <br /> Hydrology and Water Quality, Section 4.8). Compared to the groundwater in the shallow, <br /> unconfined aquifers and the semi-confined aquifers within the upper Tulare Formation, the lower <br /> Tulare Formation provides groundwater at a substantially greater quantity and with higher <br /> quality. The lower Tulare Formation provides groundwater supply for industrial uses(namely <br /> active mining operations)near the project area and municipal and industrial uses within and <br /> surrounding the city of Tracy. This analysis assumes that existing industrial operations and <br /> municipal groundwater demands would remain essentially the same, while proposed projects <br /> within the region would pump groundwater either as their primary supply or to supplement a <br /> surface water supply. As mining operations typically demand a substantial water supply for <br /> processing, dust suppression, landscaping, and domestic use,the use of groundwater for the <br /> project, in combination with other mining projects in the area, could cumulatively affect <br /> groundwater supply within the lower Tulare Formation. The cumulative affect would likely be <br /> RMC Pacific Vernalis Quarry Mining and Reclamation Project 6-12 ESA 1203015 <br /> Draft Environmental Impact Report May 20D6 <br />