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ARCHIVED REPORTS_XR0012415
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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M
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MARCH
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2701
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3500 - Local Oversight Program
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PR0545517
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ARCHIVED REPORTS_XR0012415
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Last modified
3/11/2020 11:52:06 PM
Creation date
3/11/2020 11:39:51 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012415
RECORD_ID
PR0545517
PE
3528
FACILITY_ID
FA0003798
FACILITY_NAME
MARCH LANE 76*
STREET_NUMBER
2701
Direction
W
STREET_NAME
MARCH
STREET_TYPE
LN
City
STOCKTON
Zip
95219
APN
11619007
CURRENT_STATUS
02
SITE_LOCATION
2701 W MARCH LN
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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16 ERI 205505 R02 Tosco Service Station 5886 Stockton,Califorma September 25, 2001 <br /> Based upon data collected during ongoing quarterly groundwater monitoring and sampling, dissolved <br /> hydrocarbons are effectively delineated both laterally and vertically in the vicinity of the site <br /> However, dissolved hydrocarbons continue to be detected in groundwater beneath the site and are <br /> ' concentrated in the vicinity of and downgradient of the UST cavity (Plate 2) Cumulative groundwater <br /> monitoring and sampling data are provided in Appendix C <br /> 2.2 Regional Settm <br /> The site is located within the northern San Joaquin Valley, which comprises the southern portion of the <br /> Central Valley geomorphic province of California The Sacramento Valley comprises the northern <br /> portion of the Central Valley The Central Valley is bounded by the Coast Ranges to the west and the <br /> Sierra Nevada Range to the east, and measures approximately 400 miles (northwest to southeast) by <br /> approximately 50 miles wide (Norris and Webb, 1990) <br /> The Central Valley consists of an asymmetrical syncline with the fold axis located towards the western <br /> portion of the valley and formed by sediment deposition and downwarp within the basin The lithology <br /> of the Central Valley consists of Mesozoic basement granitic and metamophic rock overlain by <br /> Cretaceous marine sedimentary rock of the Panoche Formation The Panoche Formation is overlain by <br /> a thick sequence of older Tertiary marine and then younger Tertiary non-marine sedimentary rock <br /> The surface of the valley is overlain by unconsolidated Quaternary sedimentary deposits, which <br /> originated from the erosion of the surrounding highlands and subsequent deposition within the basin <br /> (Bartow, 1985, and Norris and Webb, 1990) <br /> The Central Valley drains the interior of California through the Sacramento River drainage in the north <br /> and San Joaquin River drainage in the south Combined, these rivers account for approximately 40 <br /> jpercent of the total river discharge in California These rivers converge west of Stockton, California, <br /> to create the San Joaquin-Sacramento Delta region, which drains through the Carqinez Strait into San <br /> Francisco Bay (Norris and Webb, 1990) <br /> 4 <br />
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