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3500 - Local Oversight Program
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PR0545678
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Entry Properties
Last modified
5/20/2020 11:34:32 AM
Creation date
5/20/2020 11:22:51 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
RECORD_ID
PR0545678
PE
3528
FACILITY_ID
FA0005843
FACILITY_NAME
MASONITE CORPORATION
STREET_NUMBER
433
Direction
W
STREET_NAME
SCOTTS
STREET_TYPE
AVE
City
STOCKTON
Zip
95203
APN
14704044
CURRENT_STATUS
02
SITE_LOCATION
433 W SCOTTS AVE
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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�+ N001 <br /> Site Background Information <br /> PREM DOR <br /> 433 West Scotts Street, Stockton, California <br /> The site is located on West Scotts Avenue, approximately 250 feet east of the Lincoln Street <br /> intersection, in an industrial/commercial area of West Stockton, California(Figure 2). The site is <br /> situated in an area of low topographic relief at an elevation of approximately 10 feet above sea level <br /> (Figure 1). The property is currently occupied by the Prem Dor Corporation. <br /> REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is situated within the southern portion of the Great Valley Geomorphic Province of <br /> California, a large, elongate, northwest-trending, asymmetric structural trough; the northern and <br /> southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, <br /> respectively.The Province is bordered by the Coast Ranges to the west,the Klamath Mountains and <br /> Cascade Range to the north, and the Sierra Nevada to the east. <br /> The Great Valley has been filled with sediments derived from both marine and continental sources. <br /> Thickness of the sedimentary fill ranges from thin veneers along the valley edges to more than <br /> 20,000 feet in the south central portion of the valley.The sedimentary formations range in age from <br /> Jurassic to Recent,with the older deposits being primarily marine in origin and the younger deposits <br /> continental. Continental-derived sediments were primarily deposited in lacustrine, fluvial, and <br /> alluvial environments with sediment sources being the mountain ranges surrounding the valley.The <br /> site itself is located on unconsolidated and semi-consolidated alluvium, lake, playa, and terrace <br /> deposits of Quaternary age.Rocks composing the basement complex of the Province have not been <br /> completely defined, but are believed to be metamorphic and igneous in origin. <br /> The Modesto, Riverbank, and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin(Basin 5-22). <br /> UNDERGROUND STORAGE TANK REMOVAL <br /> It is our understanding that two underground storage tanks (USTs) were removed from the site in <br /> March 2002.The USTs were reportedly utilized for the storage and dispensing of gasoline and diesel <br /> fuel.Concentrations oftotal petroleum hydrocarbons quantified as diesel(TPH-d),gasoline(TPH-g), <br /> volatile aromatics(benzene,toluene,ethylbenzene,and xylenes:BTEX),and total lead were detected <br /> in soil samples collected from the UST excavation. <br /> Based upon the analytical results of soil samples collected during UST removal, the San Joaquin <br /> County Environmental Health Department(EHD)required the preparation of a work plan to define <br /> the lateral and vertical extents of contamination in soil and ground water. <br /> Advanced GeoEnvironmental,Inc. <br />
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