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FIELD DOCUMENTS_CASE 2
Environmental Health - Public
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FIELD DOCUMENTS_CASE 2
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Last modified
3/13/2020 10:20:03 AM
Creation date
3/10/2020 11:57:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
FIELD DOCUMENTS
FileName_PostFix
CASE 2
RECORD_ID
PR0545492
PE
3528
FACILITY_ID
FA0000309
FACILITY_NAME
MCHENRY STATION & MINI MART
STREET_NUMBER
1405
STREET_NAME
MAIN
STREET_TYPE
ST
City
ESCALON
Zip
95320
CURRENT_STATUS
02
SITE_LOCATION
1405 MAIN ST
P_LOCATION
06
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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1 <br /> i <br /> I <br /> qeo bglca I Tect"ics !`u. <br /> L 1101 7T"Street <br /> Modesto,California 95354 <br /> (209)522-4119/Fax(209)522-4227 <br /> L.l <br /> Risk Evaluation <br /> L� & <br /> Appendix B <br /> Site Closure Checklist <br /> City of Escalon — Former EZ Gas Mini-Mart <br /> 1405 Main Street <br /> Escalon, California <br /> Project No. 1114.2 <br /> September 29, 2003 <br /> 1.0 INTRODUCTION <br /> 1.1 Site Location <br /> The site, formerly EZ Gas Mini-Mart, is located at 1405 Main Street (Formerly 1405 Main <br /> Street) in Escalon, California at the intersection of McHenry Avenue and Main Street <br /> (Route 120). The Assessor's Parcel Number is 227-062-04 and is located in the Escalon <br /> Quadrangle: T2S, R9E, Sec. 4,NW 1/4,NW 1/4. <br /> 1.2 Geology and Hydrogeology <br /> The site is located on the eastern boundary of the gradually sloped floor of the northern San <br /> Joaquin Valley. The valley is approximately 400 miles long with an average width of 50 <br /> miles. The geologic composition of the area is characterized as fluvial deposits of the San <br /> Joaquin - Sacramento River delta system, which overlay continental rocks and deposits <br /> derived from erosion of the Coast Ranges to the west and the Sierra Nevada Mountain <br /> Range to the east. <br /> The southwest tilting Sierra Nevada fault block underlies the northern San Joaquin Valley <br /> area. Miocene to Holocene unconsolidated sediments, generally clays, silts and gravels, <br /> overlie the.basement granitic and metamorphic rocks. The lower consolidated batholithic <br /> and metamorphic rocks are poorly transmissive, however the overlying sedimentary layers <br /> are often quite permeable. <br />
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