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ARCHIVED REPORTS_XR0005243
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ARCHIVED REPORTS_XR0005243
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Last modified
3/10/2020 7:13:04 PM
Creation date
3/10/2020 4:22:53 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0005243
RECORD_ID
PR0545495
PE
3528
FACILITY_ID
FA0006423
FACILITY_NAME
STOCKTON MOBIL 2
STREET_NUMBER
3440
Direction
E
STREET_NAME
MAIN
STREET_TYPE
ST
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
3440 E MAIN ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Former Beacon Station No. 12474 March 18, 2002 <br /> Stockton,California Problem Assessment Report/Corrective Action Plan <br /> 3.4 REGIONAL AND LOCAL HYDROGEOLOGY <br /> The site is situated in the central portion of the Great Valley Geomorphic Province otherwise <br /> known as the Central Valley of California. The Central Valley consists of two broad, <br /> topographically distinct, alluvial valleys: the Sacramento Valley in the north; and the San <br /> Joaquin Valley in the south. These two valleys meet in the area of the inland delta formed <br /> by the confluence of the San Joaquin and Sacramento Rivers. Stockton is situated in the <br /> northern San Joaquin Valley just east of and adjacent to the San Joaquin/Sacramento River <br /> delta system. <br /> The Great Valley geomorphic province is an elongate, northwest-trending, asymmetric <br /> structural trough filled with a thick sequence of marine and non-marine sediments ranging in <br /> age from Jurassic to Holocene. Great Valley sediments generally thin to zero towards the <br /> adjacent Sierra Nevada and Coast Ranges provinces and are predominantly underlain by the <br /> westward continuation of Sierran granitic and metamorphic rocks. The Coast Ranges are <br /> • underlain, in part, by folded and faulted sedimentary rocks equivalent to intervals found at <br /> depth in the Great Valley stratigraphic sequence. <br /> Generally unconsolidated to poorly consolidated alluvial, fluvial and lacustrine deposits of <br /> Miocene to Holocene age comprise the upper portion of the stratigraphic sequence of the <br /> Great Valley province and are generally underlain by consolidated marine rocks. Surface <br /> sediments in the site area are generally Pleistocene to Holocene flood-basin deposits and <br /> Pliocene to Holocene alluvial and fluvial deposits (USGS, 1986). Lithologic data from soil <br /> borings indicate the site surface is underlain by interbedded sand, silt and clay as shown on <br /> the generalized cross sections A-A' and B-B' (Figures 3 and 4, respectively), located as <br /> shown on Figure 2. <br /> The Central Valley is divided into three hydrologic basins: the northern Sacramento River <br /> Basin, the central San Joaquin River Basin, and the southern Tulare Lake Basin. The city of <br /> • Stockton is located within the San Joaquin River hydrologic basin. The general movement <br /> 474PARCAP3-02.doc 4 <br /> Project No. 1474.23 HORIZON ENVIRONMENTAL INC. <br />
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