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ARCHIVED REPORTS_XR0010175
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545689
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ARCHIVED REPORTS_XR0010175
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Last modified
5/18/2020 4:06:43 PM
Creation date
5/18/2020 3:42:33 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0010175
RECORD_ID
PR0545689
PE
3528
FACILITY_ID
FA0005164
FACILITY_NAME
FISCO WAREHOUSE
STREET_NUMBER
1648
STREET_NAME
SHAW
STREET_TYPE
RD
City
STOCKTON
Zip
00000
CURRENT_STATUS
02
SITE_LOCATION
1648 SHAW RD
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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I <br />' Site Background Information <br /> FORMER FISCO WAREHOUSE (Howard Lenz Property) <br />' 1648 Shaw Road, Stockton, California <br /> The site is located in a commercial area of low topographic relief in east Stockton, California, at an <br />' approximate elevation of 25 feet above mean sea level. The site is bounded on the north and east by <br /> the Stockton Diverting Channel, on the west by State Highway 99 and on the south by Shaw Road. <br /> Golden West Irrigation,an agricultural irrigation supply and distributing facility,presently occupies <br /> the property. <br /> REGIONAL GEOLOGIC/HYDROGEOLOGIC 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 /> I 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 origin. <br /> The northern and southern portions of the Great Valley Province have been designated the <br /> Sacramento and San Joaquin Valleys,respectively. <br /> The Modesto,Riverbank,Turlock Lake Formations and overlying recent alluvium are therinci al <br /> P p <br /> source of domestic ground water in the 13,500-square-mile San Joaquin Valley Ground Water Basin <br /> (Basin 5-22). This basin is drained primarily by the San Joaquin River. The nearest surface water <br /> feature in the vicinity of the propertyis the Stockton Diverting Canal located approximately 300 feet <br /> north of the site. The Stockton Diverting Canal usually contains little water and has not appeared to <br /> have a significant effect upon ground water depth or flow direction in the area; however the canal <br /> could be the cause of the significant fluctuation in ground water flow direction and depth at the site. <br /> HYDROGEOLOGICAL MODEL <br /> Based on the CPT results, AGE has developed a preliminary subsurface model of the site soil <br /> stratigraphy comprised of four informal zones, a vadose (unsaturated) zone and three hydrological <br /> I units. Hydrological units may be defined as significant vertical intervals of soil having significant <br /> lateral extent and having similar hydrologic characteristics (i.e. hydraulic conductivity, <br /> transmissivity, etc.) over its vertical and horizontal extent. A `flow unit' may be defined as a <br /> hydrologic unit and is characterized by significantly greater hydraulic conductivity values than <br /> overlying and underlying units.A flow unit is capable of serving as a preferred migration route, and <br /> could potentially allow migration of large contaminant masses over great distances. <br /> IAdvanced GeoEnvironmental,Inc <br /> I ! <br />
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