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3500 - Local Oversight Program
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PR0544230
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Entry Properties
Last modified
3/5/2019 8:30:09 PM
Creation date
3/5/2019 3:51:09 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
RECORD_ID
PR0544230
PE
3528
FACILITY_ID
FA0003829
FACILITY_NAME
VANCO TRUCK-AUTO PLAZA
STREET_NUMBER
1033
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323041
CURRENT_STATUS
02
SITE_LOCATION
1033 W CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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Site Background Inf rmation <br /> VANCO TRUCK& AUTO PLAZA <br /> 1033 West Charter Way,Stockton,California <br /> i <br /> BACKGROUND <br /> I <br /> The site is situated in an area of mixed commercial and li ght industrial use,bordered by Navy Drive <br /> on the north and West Charter Way on the south.The pre minent features of the subject property are <br /> depicted on Figure 2. <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, asyminetric 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 Rang es to the west,the Klamath Mountains and <br /> Cascade Range to the north,and the Sierra Nevada to tb a 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 typi ally deposited in lacustrine, fluvial, and <br /> alluvial environments with sediment sources being the mountain ranges surrounding the valley <br /> (Olmsted and Davis, 1961); the site itself is located on unconsolidated and semi-consolidated <br /> alluvium, lake, playa, and terrace deposits of Quaternary age (California Division of Mines and <br /> Geology, 1977).Rocks composing the basement compl of the Province have not been completely <br /> defined,but are believed to be metamorphic and igneou in origin. <br /> The Modesto, Riverbank, and Turlock Lake Formatioi is and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,50 -square mile San Joaquin Valley Ground <br /> Water Basin(Basin 5-22).The depth to ground water at the site is approximately 20 feet to 25 feet <br /> below surface grade(bsg)based on information from quafterly monitoring events performed by AGE <br /> at the site;the ground water elevation is approximately 10 feet below mean sea level(MSL).Ground <br /> water generally flows toward the northeast; however, this may vary due to local recharge and <br /> discharge patterns. <br /> FUEL-DISPENSING SYSTEM UPGRADE <br /> In February 2003,as part of a fuel-dispensing system upgrade,the underground storage tank(UST) <br /> sumps,fuel dispensers,and associated piping were exca ated by the Fillner Construction Company; <br /> excavated soil was stockpiled on-site for evaluation prior to transport to Forward Landfill for <br /> Advanced GeoEnvironmental,Tne. <br />
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