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PR0530688
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Last modified
2/6/2020 2:02:45 PM
Creation date
2/6/2020 8:26:08 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0530688
PE
2950
FACILITY_ID
FA0019894
FACILITY_NAME
SJ DELTA COLLEGE - SHIMA AG
STREET_NUMBER
5151
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
APN
10816001
CURRENT_STATUS
02
SITE_LOCATION
5151 PACIFIC AVE
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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16 October 2009 <br /> AGE-NC Project No. 09-1714 <br /> Page 2 of 5 <br /> The scope of work included advancement of nineteen soil borings,for collection and analysis of soil <br /> samples, in the area of the Agricultural and Natural Resources Yard/Shima Center at SJDC, 5151 <br /> Pacific Avenue, Stockton, California. <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, asymmetric structural trough; the northern and <br /> southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, <br /> The Province is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade <br /> Range to the north, and the Sierra Nevada to the 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 /> being primarily continental. Continental-derived sediments were primarily deposited in lacustrine, <br /> fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the <br /> valley(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 complex of the Province have not been completely <br /> defined but are believed to be metamorphic and igneous in origin. <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). The estimated depth to ground water at the site is approximately 50 feet <br /> below surface grade (bsg) based on information from Lines of Equal Depth of Water Wells Fall <br /> 1999,published by the San Joaquin County Flood Control District and Water Conservation District- <br /> FCD&WCD. Based on the map titled Lines of Equal Elevation of Groundwater Spring 1999 also <br /> published by the San Joaquin County FCD&WCD, the local ground water elevation is generally <br /> toward the east. However,this may be greatly modified by local recharge and discharge patterns. <br /> PREVIOUS ENVIRONMENTAL INVESTIGATIONS <br /> In May 1995,one 2,000-gallon underground storage tank(UST),two 10,000-gallon USTs and one <br /> 500-gallon UST were removed from the site. The USTs were reportedly used for storage of waste <br /> oil associated with the adjacent shop,diesel fuel and leaded gasoline.At the time of the removal,all <br /> Advanced GeoEnvironmental,Inc. <br />
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