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MOUNTAIN HOUSE PROPOSED ALTAMONT HEIGHTS TENTATIVE MAP 4. ENviRoNMENrAL CHECKLIST <br /> 4.8 HYDROLOGY AND WATER QUALITY <br /> Less Than <br /> Potential SPU EIR Significant <br /> Significant Requires Impact Due New New <br /> Impact Additional to Mitigation Additional Additional <br /> Less Than Adequately Review:No Measures in Impact Not Mitigation <br /> Significant Addressed in Significant Project Addressed in Measures <br /> Issue or No Impact SPIHEIR Impact Description SPIIIEIR Required <br /> i) Expose people or structures to a ■ ❑ ❑ ❑ <br /> significant risk of loss,injury or <br /> death involving flooding,including <br /> flooding of as a result of the failure _ <br /> of a levee or dam? <br /> j) Inundation by seiche,tsunami,or ■ ❑ L ❑ ❑ <br /> mudflow? <br /> SETTING <br /> Climate and Topography — <br /> Average annual rainfall in the vicinity of the project site is 12 inches with most rainfall <br /> occurring from November to April. Average temperatures range from 38 degrees Fahrenheit — <br /> in winter months to 93 degrees Fahrenheit in summer months(Western Regional Climate <br /> Center, 2002). The existing topography varies from elevation 190 at the top of the small hill <br /> in the southeast corner to less,than 155 feet in the Swale at the northern boundary. <br /> Surface Hydrology <br /> A drainage Swale runs southwest to northeast across the site. An excavated drainage ditch <br /> has replaced the natural Swale in some locations. Current drainage at the site consists of <br /> overland sheet flow toward the drainage Swale and then along the Swale to the northern <br /> property boundary. A sharp bend in the Byron Bethany Irrigation District's Canal 155 is <br /> located approximately 50 feet north of the project site's northern boundary. Water in the <br /> Swale flows into the canal through a 10-inch-diameter pipe (Siegfried Engineering, 2006a). <br /> The project site is located in Watershed A-3 as defined in the SPRIEIR(EDAW, 2005b, <br /> Figure 7-1). This watershed is within the larger 15-square mile Mountain House Creek <br /> watershed. The headwaters of the creek are in the Altamont Hills approximately 6.5 miles — <br /> southwest of the Mountain House Community. The creek enters the Mountain House <br /> Community at the western boundary of Neighborhood E and flows in a northeast direction to <br /> its discharge in Old River. Runoff generated on and flowing through the project site would — <br /> drain through a storm drain system to Mountain House Creek. Runoff flowing through the <br /> project site comes from 1.9 square miles of undeveloped area southwest of the Mountain <br /> House Community that currently flows into the drainage Swale. This nmoffis considered — <br /> "clean"because it is not polluted by urban land uses. Seepage from both the Delta Mendota <br /> Canal and the California Aqueduct,located approximately 2,000 and 5,000 feet west of the <br /> project site,respectively,results in year-round water in the swale(Siegfried Engineering, <br /> 2006a). <br /> Master Drainage Plan _ <br /> Drainage improvements for the Mountain House Community are described in the Mountain <br /> House Master Drainage Plan(PACE, 2002)that was updated in the Storm Water Master Plan <br /> 4-41 <br />