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ARCHIVED REPORTS_XR0009973
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_XR0009973
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Last modified
5/20/2020 11:43:31 AM
Creation date
5/20/2020 11:37:26 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009973
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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' Site Background Information <br />' PREM DOR <br /> 433 West Scotts Street, Stockton, California <br /> The site is on West Scotts Avenue approximately 250 feet east of the intersection with Lincoln <br />' Street, in an industnal/commercial area of West Stockton(Figure 2) The site is situated in an area <br /> of low topographic relief at an estimated elevation of 13 feet above sea Ievel(Figure 1) The property <br /> 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 /> ICascade 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 /> I 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 /> being primarily continental Continental-derived sediments were primarily deposited in lacustnne, <br /> fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the <br /> valley, the site itself is located on unconsolidated and semi-consohdated alluvium, lake, playa and <br /> Iterrace deposits of Quaternary age Rocks composing the basement complex of the Province have <br /> not been completely defined but are believed to be metamorphic and igneous in origin <br /> IThe 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 /> IUNDERGROUND STORAGE TANK REMOVAL <br /> It is our understanding that two underground storage tanks (USTs) were removed from the site in <br /> I March 2002 The USTs were reportedly utilized for the storage and dispensing of gasoline and <br /> diesel Concentrations of total petroleum hydrocarbons quantified as diesel (TPH-d), gasoline <br /> (TPH-g), volatile aromatics (benzene, toluene, ethyl benzene and xylenes - BTEX) and total lead <br /> Iwere detected in soil samples collected from the UST excavation <br /> Based upon the analytical results of soil samples collected during UST removal, the EHD required <br /> the preparation of work plan to define the lateral and vertical extent of contamination in soil and <br /> ground water <br /> Advanced Geo$nvironmental,Inc <br />
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