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Environmental Health - Public
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EIGHT MILE
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2900 - Site Mitigation Program
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PR0506051
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Last modified
7/10/2019 12:26:05 PM
Creation date
7/10/2019 10:29:10 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0506051
PE
2950
FACILITY_ID
FA0007171
FACILITY_NAME
HOLIDAY HARBOR/INTREPID MARINE
STREET_NUMBER
11540
Direction
W
STREET_NAME
EIGHT MILE
STREET_TYPE
RD
City
STOCKTON
Zip
95219
APN
07119004
CURRENT_STATUS
02
SITE_LOCATION
11540 W EIGHT MILE RD
P_LOCATION
99
QC Status
Approved
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MW-6 has intermittently had low levels of toluene (12 to 38 µg19) since it was installed. Ethylbenzene and <br /> ' xylenes were detected during the March 1994 sampling event at 8.8 and 33 µg19 respectively. <br /> SECOR conducted a Phase I Environmental Site Assessment of the site in July 1995. At the time of the initial <br /> ' inspection,there were seven USTs (two gasoline,five septic)on the King Island property. <br /> Based on previous investigations,SECOR recommended that a soil and groundwater investigation be conducted <br /> ' on both the King Island and Holiday Harbor portions of the site. This report outlines the details of the <br /> investigation. <br /> ' 1.3 REGIONAL GEOLOGIC AND HYDROGEOLOGIC CONDITIONS <br /> - The site is located on King Island, within the Sacramento River Delta. The primary structural features in this <br /> region are the Midland Fault Zone located 10 miles west of the site and the Stockton Fault located <br /> approximately 15 miles to the south. The Midland Fault Zone trends northwest/southeast and the Stockton <br /> Fault trends northeast/southwest. Based on information obtained from the United States Geological Survey's <br /> Geology of the Fresh Groundwater Basin of the Central Valley, the site lies on Holocene flood basin deposits. <br /> ' Soil in the area includes mud, peat, muck, loam, and lesser amounts of silt and sand. <br /> Groundwater in the vicinity of the site flows in a general northeast direction from Honker Cut towards Lodi. <br /> ' Regionally, groundwater typically flows away from the levees towards the lower lying areas and is also <br /> influenced by tidal fluctuations. A primary use of surface water in the Delta region is irrigation of agricultural <br /> land, and is controlled by irrigation ditches found throughout the region. Local variations in groundwater flow <br /> ' exist which are related to topography and the geometry of local aquifers. Depth to groundwater in the area <br /> ranges from 2 to 12 feet below ground surface(bgs). <br /> 1 <br /> ' Soi7�-oofm <br />
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