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ARCHIVED REPORTS_XR0010419
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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3500 - Local Oversight Program
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PR0545067
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ARCHIVED REPORTS_XR0010419
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Last modified
12/12/2019 10:13:30 AM
Creation date
12/12/2019 9:39:39 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0010419
RECORD_ID
PR0545067
PE
3526
FACILITY_ID
FA0005019
FACILITY_NAME
BANNER ISLAND BALLPARK
STREET_NUMBER
404
Direction
W
STREET_NAME
FREMONT
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
13741017
CURRENT_STATUS
02
SITE_LOCATION
404 W FREMONT ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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404 WEST FREMONT <br /> t WKA No 1628 01 <br /> February 25, 1993 <br /> Page 4 <br /> The soil and ground water contamination is reported to be located beneath two areas of the Chase <br /> Chevrolet property near the northeast corner of Fremont and Madison Street, and near the <br />' western border along Van Buren Street The contamination along Van Buren Street is a concern <br /> due to the high levels of gasoline contamination detected in ground water samples from the three <br /> monitoring wells located there, and the proximity of the contamination to the Crystal Creamery <br />' property One of the three wells is reported by RESNA in their April 16, 1992 Quarterly <br /> Report, to have over 11/z feet of floating hydrocarbons on the water The RESNA quarterly <br />' report also indicates ground water flow direction beneath the western portion of the property is to <br /> the north with a gradient of 0 003 ft/ft <br /> 1 <br /> Hydrogeologic Setting <br /> The 1966 California Division of Mines and Geology "Geologic Map of California, San Jose <br /> Sheet" shows the site to be underlain by Quaternary Basin Deposits These deposits consists <br /> primarily of "semi-consolidated gravels, sands and silts" that are the remnants of older alluvial <br /> terraces and dissected alluvial fans The thickness of the Quaternary Basin Deposits is variable <br /> but is likely to be over one hundred feet thick beneath the site The soils observed during the <br />' tank removal were brown and gray sands and silts <br />' The site heb within the San Joaquin Valley Ground Water Basin (California Department of Water <br /> Resources, 1986) The upper ground water table is expected to be unconfined and approximately <br /> 20 feet below grade, based on the Spring, 1990 Ground Water Elevation Contour Map published <br /> by San Joaquin Flood Control and Water Conservation District The regional ground water flow <br /> direction is reported to be easterly, ground water depths have been observed to fluctuate between <br />' 16 to 27 feet below grade <br /> WALLAC5 ILUML <br /> R.>,I�d p„p,T 6 ASSOCIA755 IWC. <br />
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