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SU0006253 SSCRPT
Environmental Health - Public
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SU0006253 SSCRPT
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Last modified
12/13/2019 10:26:09 AM
Creation date
9/5/2019 10:46:33 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0006253
PE
2611
FACILITY_NAME
PA-0600363
STREET_NUMBER
20058
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
MOUNTAIN HOUSE
APN
20907026
ENTERED_DATE
9/15/2006 12:00:00 AM
SITE_LOCATION
20058 W GRANT LINE RD
RECEIVED_DATE
9/12/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\sballwahn
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\MIGRATIONS\G\GRANT LINE\20058\PA-0600363\SU0006253\SSC RPT.PDF
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EHD - Public
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KLEINFELDER <br /> r <br /> 3.2. SITE AND VICINITY GENERAL CHARACTERISTICS <br /> The site is located in an area of relatively level terrain. Land onsite was an uncultivated field <br /> r with a rural residence at the time of Kleinfelder's assessment. Groundwater information is <br /> included on Table 2 below. <br /> TABLE 2 <br /> GROUNDWATER INFORMATION <br /> 1 � k <br /> DEPTH TU'REGIONAL ' ' w t t ' Based upon the State of California, Department of Water Resources <br /> GROUNDWATER AND Sao , `A. �.. (DWR) for well records in the surrounding area. Groundwater <br /> GROUNDWATER FLOW DIRECTION V contours have not been plotted in the vicinity of the City of Tracy <br /> (Source State of California,Department aft' due to the inconsistent data and the nature of the aquifers. However, <br /> Water Resources, 'N �, the regional direction of groundwater flow is expected to follow <br /> *. s = surface topography, generally to the west-northwest. Depths to <br /> a Internet Website fs subsurface and/or perched water zones are anticipated to be relatively <br /> v http]/well water ca�ov} " '4 shallow in the lower areas of the site and relatively deeper in the <br /> hilltop areas. According to the San Joaquin County Environmental <br /> Health.Department, water levels recorded from a well along Grant <br /> is Line Road approximately 400 feet from the San Joaquin-Alameda <br /> County border in October of 2003 are at 32 feet below ground <br /> (bgs). Groundwater flow direction and depth may be <br /> a _ influenced by local geology,pumping,rainfall and irrigation patterns. <br /> of such factors is beyond the scope of this re ort. <br /> 3.3. CURRENT/PROPOSED USE OF THE PROPERTY <br /> r <br /> Current and proposed uses are described in Table 3. <br /> #.; TABLE 3 <br /> y CURRENT/PROPOSED USES <br /> CURRENT'USE3 ' Uncultivated field with a rural residence. <br /> t PROPO$ED;VSE= ',Y; Commercial development. <br /> Ott <br /> 1 l <br /> f <br /> L <br /> 55568.P01/STO5R488R/LTV:Iv Page 7 of 30 <br /> ©2005 Kleinfelder,Inc. June 1,2005 <br /> i� <br />
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