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2900 - Site Mitigation Program
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PR0505804
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Last modified
1/31/2020 5:47:42 PM
Creation date
1/31/2020 4:02:09 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0505804
PE
2960
FACILITY_ID
FA0007013
FACILITY_NAME
KOPPEL STOCKTON TERMINAL
STREET_NUMBER
2025
Direction
W
STREET_NAME
HAZELTON
STREET_TYPE
AVE
City
STOCKTON
Zip
95203
CURRENT_STATUS
01
SITE_LOCATION
2025 W HAZELTON AVE
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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31 January 2000 <br /> AGE-NC Project No. 99-0653 <br /> Page 2 of 6 <br /> TPH as gasoline were not reported in soil samples collected. A summary of soil analytical results <br /> are presented in Table 1. <br /> 2.3. 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(Olmsted 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 /> 2.4. GROUND WATER DEPTH AND FLOW DIRECTION <br /> Based on data obtained from wells on the property, depth to ground water at the site is between 6 and <br /> 10 feet below surface grade(bsg). The prevailing ground water flow direction in the vicinity of the <br /> site is southwest. However, flow direction may be both locally and seasonably variable. <br /> 3.0. SCOPE OF WORK <br /> In a letter dated 27 September 1993, the San Joaquin County Public Health Services - Environmental <br /> Health Division (PHS-EHD)stated that the site could not be evaluated for closure without additional <br /> information. AGE proposes to collect soil and grab ground water samples to evaluate the lateral and <br /> vertical extent of the inferred petroleum hydrocarbon impact. The preliminary subsurface <br /> investigation will consist of the following tasks: <br /> Advanced GeoEm ironmental,Inc. <br />
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