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SITE HISTORY
Environmental Health - Public
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EHD Program Facility Records by Street Name
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WILSON
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821
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2900 - Site Mitigation Program
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PR0540773
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SITE HISTORY
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Last modified
7/8/2020 3:05:21 PM
Creation date
7/8/2020 3:00:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE HISTORY
RECORD_ID
PR0540773
PE
2960
FACILITY_ID
FA0023307
FACILITY_NAME
FORMER OCAMPO PROPERTY
STREET_NUMBER
821
Direction
S
STREET_NAME
WILSON
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
CURRENT_STATUS
01
SITE_LOCATION
821 S WILSON WAY
P_LOCATION
01
QC Status
Approved
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EHD - Public
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y _ <br /> Site Background Information <br /> Former OCAMPO PROPERTY <br /> 821 South Wilson Way, Stockton, California <br /> The site is located at the northeast corner of the intersection between East Taylor Street <br /> and South Wilson Way Frontage Road in the south central portion of the City of Stockton, <br /> San Joaquin County, California. It is situated in an area of mixed commercial, light <br /> industrial, and residential use. The site is currently occupied by tenants who live onsite and <br /> are involved in rebuilding vehicles and recycling. <br /> REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is situated within the Great Valley Geomorphic Province of California, a large, <br /> elongate, northwest-tending, asymmetric structural trough. The Great Valley Province has <br /> been filled with thick sequences of sediment ranging in age from Jurassic to Recent, <br /> creating a nearly flat-lying alluvial plain, which extends from the Tehachapi Mountains in <br /> the south to the Klamath Mountains in the north. The western and eastern boundaries of <br /> this province are comprised of the California Coast Range and the Sierra Nevada, <br /> respectively. Rocks composing the basement complex of the province have not been <br /> completely defined but are believed to be of metamorphic and igneous origin. The Great <br /> Valley Province has been subdivided into two majordivisions, identified as the Sacramento <br /> and San Joaquin Valleys. <br /> The Modesto, Riverbank, and Turlock Lake Formations and overlying Recent alluvium are <br /> the principal sources of domestic ground water in the 13,500-square mile San Joaquin <br /> Valley Ground Water Basin (Basin 5-22). This basin is drained primarily by the San <br /> Joaquin River. The actual depth to groundwater at the site is 40 to 45 feet below surface <br /> grade (bsg), based on the depth to water measurements from wells installed on-site. The <br /> nearest surface water feature in the vicinity is the Mormon Slough, approximately 1,200 <br /> feet south of the site. <br /> UNDERGROUND STORAGE TANK REMOVAL <br /> It is AGE's understanding that a single 550-gallon underground storage tank (UST) was <br /> removed from the site by Kleinfelder & Associates on December 18, 1985. A soil sample <br /> collected from under the UST after removal indicated that high concentrations of lead were <br /> present. <br /> Advanced GeoLnvironmental,Inc. <br />
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