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ARCHIVED REPORTS_XR0009942
Environmental Health - Public
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EHD Program Facility Records by Street Name
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S
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SCOTTS
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433
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3500 - Local Oversight Program
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PR0545678
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ARCHIVED REPORTS_XR0009942
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Last modified
5/20/2020 11:43:13 AM
Creation date
5/20/2020 11:36:09 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009942
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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I <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 /> I principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22) <br /> IUNDERGROUND 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 /> IBased 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 /> Ithe lateral and vertical extents of contamination in soil and ground water <br /> Advanced GeoEnv►ronmeotal,Inc <br />
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