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SU0008578
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SU0008578
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Last modified
5/7/2020 11:33:34 AM
Creation date
9/5/2019 11:09:22 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0008578
PE
2611
FACILITY_NAME
PA-1000266
STREET_NUMBER
18500
Direction
S
STREET_NAME
HENDERSON
STREET_TYPE
RD
City
TRACY
APN
20917004
ENTERED_DATE
1/7/2011 12:00:00 AM
SITE_LOCATION
18500 S HENDERSON RD
RECEIVED_DATE
1/7/2011 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\H\HENDERSON\18500\PA-1000266\SU0008578\APPL.PDF \MIGRATIONS\H\HENDERSON\18500\PA-1000266\SU0008578\CDD OK.PDF \MIGRATIONS\H\HENDERSON\18500\PA-1000266\SU0008578\EH COND.PDF \MIGRATIONS\H\HENDERSON\18500\PA-1000266\SU0008578\EH PERM.PDF
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EHD - Public
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MOUNTAIN HOUSE NEIGHBORHOODS K AND L INITIAL STUDY 5.ENVIRONMENTAL CHECKLIST <br /> B.HYDROLOGY AND WATER QUALITY <br /> � ) 700-Year Floodplain <br /> Current Federal Emergency Management Agency(FEMA) maps for San Joaquin <br /> County designate roughly half of Neighborhoods K and L(the portions of the site <br /> located at or below 10 feet above msl)as being within the 100-year flood hazard <br /> zone for Old River(see Figure 5.8-1). The flood zone forms a band about 1,500 <br /> #� to 2,000 feet wide along the Old River levee at the northern edge of the Mountain <br /> House community(FEMA, 2009). <br /> Groundwater <br /> The Department of Water Resources(DWR)defines state groundwater basins <br /> L based on geologic and hydrogeologic conditions. According to the DWR, <br /> Neighborhoods K and L are located within the Tracy groundwater subbasin. The <br /> subbasin has an area of approximately 540 square miles and is drained by the <br /> San Joaquin River and Corral Hollow Creek. Primary water-bearing formations <br /> in the subbasin include semi-consolidated deposits of clay, silt, and gravel of the <br /> Tulare Formation,flood basin deposits, and older and younger alluvium(DWR, <br /> 2006). <br /> Generally, groundwater flows as a subdued reflection of the surface topography. <br /> Hydrographs for the Tracy groundwater subbasin indicate that the majority of <br /> water levels in wells within the subbasin have remained relatively stable over <br /> F ' time(DWR,2006). During subsurface investigations conducted in 2007 and <br /> 2010,groundwater was encountered in all soil borings in Neighborhood K at <br /> depths of 3 to 12 feet below the ground surface (bgs)and in Neighborhood L at <br /> 4.5 to 14.5 feet bgs(Engen, 2007, 2010). <br /> The water quality of the Tracy groundwater subbasin is somewhat impaired. <br /> Areas of poor water quality exist throughout the subbasin and elevated levels of <br /> chloride and nitrate have been encountered in the vicinity of the City of Tracy. <br /> According to the 1994 MEIR, elevated levels of total dissolved solids(TDS), <br /> nitrates, and sulfides have been encountered in groundwater in and around the <br /> Mountain House community.The high levels of TDS may be the result of <br /> saltwater intrusion from the Delta. Relatively high levels of nitrates may be the <br /> result of poor livestock management in the surrounding area and/or releases <br /> from household septic systems. <br /> Project Studies <br /> i The applicant has completed the following studies related to storm water <br /> L ' drainage for Neighborhoods K and L: <br /> (7 ■ Pacific Advanced Civil Engineering(PACE), Inc.,April 2002, Master <br /> Drainage Plan. <br /> Pacific Advanced Civil Engineering (PACE), Inc., September 28,2006. <br /> Storm Wafer Master Plan Update,Addendum Il. <br /> 010 <br /> Fill (quill) 5-105 <br />
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