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ARCHIVED REPORTS XR0010469
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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DR MARTIN LUTHER KING JR
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749
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3500 - Local Oversight Program
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PR0544218
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ARCHIVED REPORTS XR0010469
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Last modified
3/5/2019 12:30:48 PM
Creation date
3/5/2019 10:16:41 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0010469
RECORD_ID
PR0544218
PE
3526
FACILITY_ID
FA0003870
FACILITY_NAME
SRH FOOD & GAS
STREET_NUMBER
749
Direction
E
STREET_NAME
DR MARTIN LUTHER KING JR
STREET_TYPE
BLVD
City
STOCKTON
Zip
95206
APN
14734309
CURRENT_STATUS
02
SITE_LOCATION
749 E DR MARTIN LUTHER KING JR BLVD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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RECENT FIELD WORK <br /> 1 <br /> Between July 29th and August 3rd, 1993 we drilled two additional <br /> wells at this site and one boring. The wells were drilled to <br /> a depth of 65 feet and 2 inch Schedule 40 PVC slotted (0 .02) <br /> casing was placed from the well bottom upward 20 feet. The <br /> remaining casing was 2" blank schedule 40 PVC and was placed <br /> to the surface. Number 3 sand was placed opposite the slotted <br /> section and about 20 feet above the last slot. Then the <br /> r annulus was filled with hydrated bentonite for 3 feet and the <br /> remainder of the annulus was sealed with neat cement. A <br /> traffic box was placed over the well and cemented to the <br /> pavement. (See Well Logs. ) <br /> The wells were developed by removing approximately 70 gallons of <br /> water at which time the sediment was greatly reduced. <br /> Approximately 24 to 48 hours later, the wells were surveyed, <br /> with a spirit level, to tie the tops of the casings to the local <br /> datum, measured for depth to water, and sampled. ( See <br /> Protocols) <br /> i <br /> SITE CHARACTERIZATION <br /> GEOLOGY <br /> The site and all nearby terrain are underlain by non-marine, <br />• fine-grained sediments which are tentatively assigned to the <br /> Modesto Formation of Pleistocene age. (USGS Bulletin 1470 <br /> Marchand and Alwordt, 1981) . Although the Modesto is typically <br /> composed of coarser-grained material such as sands and gravels <br />• it is reasonable, on the basis of stratigraphic position, to <br /> consider these finer-grained sediments to be the distal portion <br /> of the large alluvial fans which make up the Modesto. <br /> The materials penetrated in our borings are chiefly clay, silty <br />• <br /> clay and clayey silt. Sandy strata, although present, are <br /> Page 4 <br />• <br />
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