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2900 - Site Mitigation Program
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PR0516371
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Last modified
7/2/2020 9:39:15 PM
Creation date
7/2/2020 10:01:55 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
COMPLIANCE INFO
RECORD_ID
PR0516371
PE
2950
FACILITY_ID
FA0012583
FACILITY_NAME
MANNYS RESTAURANT
STREET_NUMBER
7925
STREET_NAME
THORNTON
STREET_TYPE
RD
City
STOCKTON
Zip
95207
APN
07522041
CURRENT_STATUS
01
SITE_LOCATION
7925 THORNTON RD
P_LOCATION
99
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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02 August 2000 <br /> AGE-NC Project No. 00-0728 <br /> Page 2 of 6 <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 the San Joaquin County Flood Control District and Water Conservation District Lines of <br /> Equal Depth of Water Wells Fall 1998 map, the estimated depth to ground water in the vicinity of <br /> the site is 30 to 40 feet below surface grade (bsg). <br /> Based upon data obtained from nearby sites, the prevailing ground water flow direction in the <br /> vicinity of the site is estimated to be southeast. However, flow direction may be both locally and <br /> seasonably variable. <br /> 3.0. SCOPE OF WORK <br /> AGE proposes to collect soil and discrete ground water samples to determine if petroleum <br /> hydrocarbon-impacted soil and/or ground water is present beneath the site. The preliminary site <br /> assessment will consist of the following tasks: <br /> • Permitting and pre-field work activities; <br /> • Soil sample collection and analysis; <br /> Advanced GeoEnvironmental,Inc. <br />
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