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TILLIE LEWIS
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2900 - Site Mitigation Program
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PR0516538
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Last modified
5/8/2020 2:01:12 PM
Creation date
5/8/2020 1:53:48 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0516538
PE
2950
FACILITY_ID
FA0005401
FACILITY_NAME
EVERGREEN GLASS INC
STREET_NUMBER
1444
STREET_NAME
TILLIE LEWIS
STREET_TYPE
DR
City
STOCKTON
Zip
95206
APN
16335003
CURRENT_STATUS
01
SITE_LOCATION
1444 TILLIE LEWIS DR
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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04 Ocotber 2000 <br /> AGE-NC Project No. 00-0768 <br /> Page 3 of 7 <br /> 2.4. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is located within the northern San Joaquin Valley which comprises part of the Great Valley <br /> geomorphic province of California. The San Joaquin Valley is formed by the Great Valley <br /> geosyncline,which is a large, elongate, northwest-trending asymmetrical structural trough(basin). <br /> It is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade Range to the <br /> north, and the Sierra Nevada to the east. This trough has been filled with sediments derived from <br /> both marine and continental sources. Thickness of the sedimentary fill ranges from thin veneers <br /> along the valley edges to more than 20,000 feet in the south central portion of the valley. The <br /> sedimentary formations range in age with the older deposits being primarily marine in origin and the <br /> younger deposits being primarily continental. Continental-derived sediments were primarily <br /> deposited in lacustrine, fluvial, and alluvial environments with sediment sources being the mountain <br /> ranges surrounding the valley(Ohnsted and Davis, 1961). The site is located on unconsolidated and <br /> semi-consolidated alluvium, lake,playa and terrace deposits of Quaternary age(California Division <br /> of Mines and Geology, 1977). <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 /> 2.5. GROUND WATER DEPTH AND FLOW DIRECTION <br /> The estimated depth to ground water at the site is 10 feet below surface grade (bsg) based on <br /> information from Lines of Equal Depth of Water Wells Fall 1996, published by the San Joaquin <br /> County Flood Control District and Water Conservation District-FCD&WCD, and data from nearby <br /> sites. Based on the map titled Lines of Equal Elevation of Groundwater Spring 1996 also published <br /> by the San Joaquin County FCD&WCD,the site is in an area where ground water flows toward the <br /> southeast. <br /> 3.0. SCOPE OF WORK <br /> AGE proposes to collect soil and discrete ground water samples to determine if petroleum <br /> hydrocarbon and/or MTBE-impacted soil and/or ground water is present beneath the site. The phase <br /> II site assessment will consist of the following tasks: <br /> • Permitting and pre-field work activities; <br /> • Soil sample collection and analysis; <br /> Advanced CeoEnvironmental,Inc. <br />
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