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ARCHIVED REPORTS_XR0008086
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0542364
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ARCHIVED REPORTS_XR0008086
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Last modified
5/4/2020 3:45:23 PM
Creation date
5/4/2020 3:22:58 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008086
RECORD_ID
PR0542364
PE
2960
FACILITY_ID
FA0024340
FACILITY_NAME
PACIFIC CAR WASH
STREET_NUMBER
4405
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
APN
11024014
CURRENT_STATUS
01
SITE_LOCATION
4405 PACIFIC AVE
P_LOCATION
01
QC Status
Approved
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LSauers
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EHD - Public
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. 15 February 2002 <br /> AGE-NC Protect No 96-0229 <br /> Page 4of12 <br /> 23 REGIONAL GEOLOGIC SETTING <br /> The property is situated within the Great Valley Geomorphic Province of California, a large, <br /> elongate, northwest trending, asymmetric structural trough The Great Valley Province has been <br /> filled with thick sequences of sediment ranging in age from Jurassic to Recent, creating a nearly flat- <br /> lying alluvial plain, extending from the Tehachapi Mountains in the south to the Klamath Mountains <br /> In the north The western and eastern boundaries of this province are comprised of the California <br /> Coast Range and the Sierra Nevada, respectively Rocks composing the basement complex of the <br /> province have not been completely defined but are believed to be metamorphic and igneous in origin <br /> The northern and southern portions of the Great Valley Province have been designated the <br /> Sacramento and San Joaquin Valleys, respectively <br /> Based on the General Soil Map from the San Joaquin County Soil Survey, published by the United <br /> States Department of Agriculture Soil Conservation Service in 1992, the site area is within the <br /> Jackson-Hallenbeck-Stockton (JHS) association The JHS soils are located within basins, and <br /> generally consist of moderate to poorly drained fine textured soils The soils are generally derived <br /> from both marine and non-marine sediment, and are generally formed In alluvium denved from <br /> • mixed rock sources <br /> 2 4 GROUND WATER DEPTH AND GRADIENT <br /> The estimated depth to ground water at the site is approximately 30 feet below surface grade (bsg) <br /> based on information from Lines of Equal Depth of Water Wells Fall 1999, published by the San <br /> Joaquin County Flood Control District and Water Conservation District(SJCFCD) Based on review <br /> of a regional ground water elevation map published by the SJCFCD, the prevailing ground water <br /> flow direction in central Stockton is generally toward the northeast, although flow directions may <br /> be both locally and seasonably variable <br /> Based on ground water monitoring data collected at the site on 31 December 2001, depth to ground <br /> water at the site was recorded at approximately 30 feet bsg and ground water flow direction was <br /> inferred to be flowing towards the northeast at a gradient of 0 001 ft/ft <br /> 3.0. SCOPE OF WORK <br /> AGE proposes to drill and install seven wells screened through the First Water Zone (located <br /> between 20 and 45 feet bsg) one 6-inch diameter ground water extraction well (EW-1) will be <br /> screened between 20 feet and 45 feet bsg, three 4-Inch diameter SVE wells (VW-1, VW-2 and <br /> VW-3) will be screened between 10 and 30 feet bsg, one 2-inch diameter IAS well (AW-1) will be <br /> Advanced GeoEnvironmental,Inc <br />
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