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2900 - Site Mitigation Program
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PR0529434
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Entry Properties
Last modified
2/17/2026 2:14:55 PM
Creation date
2/17/2026 2:01:08 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0529434
PE
2959 - DTSC LEAD AGENCY SITE
FACILITY_ID
FA0019555
FACILITY_NAME
SOUTH POINTE DEVELOPMENT SITE (CITY OF STKN REDEVELOPMENT AGENCY)
STREET_NUMBER
701
Direction
W
STREET_NAME
WEBER
STREET_TYPE
AVE
City
STOCKTON
Zip
95202
APN
13726016
CURRENT_STATUS
Active, billable
QC Status
Approved
Scanner
SJGOV\gmartinez
Supplemental fields
Site Address
701 W WEBER AVE STOCKTON 95202
Tags
EHD - Public
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SUPPLEMENTAL SITE INVESTIGATION WORK PLAN <br /> South Pointe Property <br /> Stockton,California <br /> Site Background <br /> 2.2 SITE GEOLOGY AND HYDROGEOLOGY <br /> The site is located within the Great Valley geomorphic province, a large, elongate, northwest- <br /> trending structural trough bounded to the west by the Coast Ranges and to the east by the <br /> Sierra Nevada.The Great Valley consists of two long north-south trending valleys connected <br /> end-to-end, with the Sacramento Valley to the north and the San Joaquin Valley to the south. <br /> The site is located in the northern portion of the San Joaquin Valley. <br /> The Sacramento and San Joaquin Valleys have been filled with thick sequences of sediment <br /> derived from marine and continental sources. Sedimentary deposits are relatively thin at the <br /> valley edges and thicken to more than 25,000 feet in the deepest interior areas. In general, older <br /> formations are marine in origin, and younger formations are derived from continental sediments. <br /> Younger sediments are being continually eroded, primarily from the Sierra Nevada, and <br /> transported to the valleys by downslope fluvial systems. <br /> Previous geotechnical and environmental investigations have identified shallow soils beneath <br /> the site as consisting of native sandy materials mixed heterogeneously with rubble and debris <br /> associated with historical building foundations and similar relics of historical site use. Deeper <br /> native soils consist primarily of fine-grained sand to depths of 10 to 15 feet below ground surface <br /> (ft bgs). Groundwater has historically been encountered at depths ranging from 8 to 17 ft bgs. <br /> Previous environmental investigations associated with the L&M Operable Unit site located south <br /> of the subject property have identified an 'A' groundwater zone at 15 to 30 ft bgs and a 'B' <br /> groundwater zone at 48 to 53 ft bgs. <br /> PREVIOUS SITE INVESTIGATIONS <br /> The following sections describe previous environmental investigations at the site. <br /> 2.2.1 Geotechnical Assessment - 2006 <br /> In September and October 2006, Neil O. Anderson and Associates performed a geotechnical <br /> investigation of the site which consisted of advancing 14 exploratory soil borings to depths <br /> ranging from 16.5 to 41.5 ft bgs. Encountered materials consisted of loose to well-compacted <br /> sandy clay, sandy gravel, and clayey sand mixed with gravel, concrete, and brick debris to <br /> depths ranging from 3 to 16 ft bgs. The investigation identified the widespread presence of <br /> concrete debris beneath the site, including buried foundations and underground structures, and <br /> recommended these materials be removed during site redevelopment and resulting voids filled <br /> with appropriate fill. Additionally, onsite native soils were deemed appropriate for use as <br /> engineered fill, but that this fill should be free of vegetation and deleterious material. <br /> 2.2.2 Environmental Assessment - 2007 <br /> Wallace-Kuhl & Associates, Inc. (WKA) performed a site-wide investigation and published the <br /> results in the document entitled Subsurface Investigation Report, Stockton Promenade & <br /> 2.2 <br />
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