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2900 - Site Mitigation Program
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PR0506525
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Last modified
10/24/2018 10:03:43 PM
Creation date
10/24/2018 2:11:53 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0506525
PE
2960
FACILITY_ID
FA0007475
FACILITY_NAME
MCMULLIN DEHYDRATOR STATION
STREET_NUMBER
26250
Direction
S
STREET_NAME
AIRPORT
STREET_TYPE
WAY
City
MANTECA
Zip
95336
APN
25703010
CURRENT_STATUS
01
SITE_LOCATION
26250 S AIRPORT WAY
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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Lj <br />Section 3 <br />• <br />REGIONAL GEOLOGIC AND HYDROGEOLOGIC SETTING <br />The McMullin Gas Dehydrator Station is located in the San Joaquin Valley with the Great Valley <br />Geomorphic Province. The San Joaquin Valley is a northwestward -trending, asymmetric structural basin <br />bounded on the east by the Siena Nevada Range and the west by the Coast Ranges. Locally, this basin <br />has been infilled with up to 6 vertical miles of both marine and non -marine rocks and sediments that <br />range in age from Jurassic (about 160 million years ago) to Holocene (the past 11,000 years). Geologic <br />maps of the San Joaquin Valley prepared by Page (1986) show the site is immediately underlain by flood <br />plain deposits of Holocene age. These deposits consist predominantly of clay and silt with some <br />interbedded sands. Geologic cross sections through the area show that the flood plain deposits are <br />underlain by lacustrine and marsh deposits of Pliocene to Holocene age (i.e., younger than 5 million <br />years). The lacustrine deposits include a relatively thick and regionally extensive clay unit, referred to as <br />the E -clay, which is present beneath the site between the approximate depths of 200 to 300 feet <br />(Page 1986). Older rocks and sediments of continental and marine origin underlie the lacustrine and <br />marsh deposits. <br />This facility is also located in the Eastern San Joaquin County Groundwater Basin (CDWR 1980). A <br />regional groundwater potentiometric surface map prepared by the San Joaquin County Flood Control <br />District for Fall 1973 shows that groundwater occurs at an elevation of about 10 feet above mean sea <br />level and flows to the west-northwest. This is consistent with the groundwater elevation data collected at <br />the site by CH2M Hill in late 1997. Recharge to the basin occurs along the foothills of the Sierra Nevada <br />Range at the eastern boundary of the basin, and from surface infiltration. Discharge from the basin <br />occurs through drainage into the San Joaquin River, a gaining river in the Tracy -Manteca area, and from <br />extensive groundwater withdrawal in the area of Stockton. <br />402 331-98 63 3-1 <br />
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