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ARCHIVED REPORTS_XR0003092
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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JACKSON
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1702
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3500 - Local Oversight Program
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PR0545315
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ARCHIVED REPORTS_XR0003092
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Last modified
2/11/2020 11:45:06 AM
Creation date
2/11/2020 9:50:15 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003092
RECORD_ID
PR0545315
PE
3528
FACILITY_ID
FA0003572
FACILITY_NAME
DAVES UNION SERVICE
STREET_NUMBER
1702
STREET_NAME
JACKSON
STREET_TYPE
ST
City
ESCALON
Zip
95320
APN
227-14-011
CURRENT_STATUS
02
SITE_LOCATION
1702 JACKSON ST
P_LOCATION
06
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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This well was located visually, however the DWR files contained no records of this well The <br /> information provided by DWR did not provide accurate locations of any of the nearby wells <br /> 3.0 REGIONAL GEOLOGY AND HYDROLOGY <br /> The site is situated in central Escalon 1n Section 4, T2S, R9E, San Joaquin County, California <br /> Regionally the property is located in the San Joaquin Valley physiographic province The valley <br /> is a topographic and structural basin bounded on the east by the Sierra Nevada and on the west <br /> by the Coast Ranges Locally the topography slopes gently toward the west at approximately <br /> 5 feet per mile <br /> The near surface geology underlying the site is comprised of unconsolidated alluvial deposits of <br /> ' Pleistocene to Holocene age These deposits, sometimes referred to as the "older alluvium", <br /> consist of intercalated beds of gravel, sand, silt and clay The thickness of the older alluvium <br /> in the Escalon area averages approximately 450 feet Underlying the older alluvium are <br /> Plio/Pleistocene continental deposits of similar derivation and lithology The older alluvium <br /> functions as the most important aquifer in the site area (USGS Professional Paper 1401-C, <br /> 1986) Soils developed on the alluvium are generally well drained, differing from the parent <br /> material only in the increased volume of organic matter (DWR Bulletin No 146, 1967) <br /> The important bodies of surface water in proximity to the site are the Stanislaus, Tuolumne, and <br /> San Joaquin Rivers The Stanislaus and Tuolumne Rivers, respectively, are located <br /> ' approximately 2 112 and 10 1/2 miles south of the site These two rivers flow in a westerly <br /> direction and are tributaries to the San Joaquin River, located approximately 14 miles west of <br /> the site The northerly flowing San Joaquin River drains the San Joaquin Valley All three of <br /> these rivers are gaining streams over portions of the year and derive a portion of their flow from <br /> ' groundwater influx (USGS Professional Paper 1401-C, 1986) Existing and potential beneficial <br /> uses of these surface water bodies include minimal and domestic water supply, irrigation, <br /> ' industrial supply, groundwater recharge, freshwater replenishment, hydroelectric power, <br /> 1500471RFMR'MCAP 0694 FNL 2 <br />
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