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ARCHIVED REPORTS XR0011121
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3500 - Local Oversight Program
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PR0544222
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ARCHIVED REPORTS XR0011121
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Entry Properties
Last modified
3/5/2019 4:41:23 PM
Creation date
3/5/2019 2:37:20 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011121
RECORD_ID
PR0544222
PE
3528
FACILITY_ID
FA0005976
FACILITY_NAME
TIRE & WHEEL MASTERS
STREET_NUMBER
814
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16718101
CURRENT_STATUS
02
SITE_LOCATION
814 E CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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Monla Brothers Service Station 12 July 16, 1992 <br /> T k <br /> 2 <br /> sin 4e—g oundwater--monitoring—wed—located—down—gradient--from—•the--loca onof t <br /> mer—gam ne tank <br /> Site Geology <br /> The subject property is located east of the San Joaquin delta near the northern end of <br /> the San Joaquin Valley This area consists of a thick sequence of fine to coarse <br /> sediments Regionally, the property is located in the San Joaquin sub-basin of the <br /> ' geomorphic province known as the Great Valley This province is characterized by a <br /> northwest-trending asymmetric structural trough bounded on the east by the Sierra <br /> Nevada Province and on the west by the Coast Range Province The Great Valley is <br /> composed of a thick sequence (60,000 feet) of sedimentary rocks ranging in age from <br /> Jurassic (205 - 138 million years ago) to Recent (10,000 years ago) and overlies a <br /> ' metamorphic and igneous basement complex (Bailey, et al, 1964) Jurassic, <br /> Cretaceous (138 - 63 million years ago) and Tertiary (63 - 2 million years ago) rocks <br /> are predominantly of marine origin (Knoxville Formation, Shasta Series, Chico <br /> Group) Tertiary sediments are almost entirely clastic, and were largely derived from <br /> ' the eroding Sierra Nevada Tectonism beginning in the upper Miocene (24 - 5 <br /> million years ago) and continuing to the present has resulted in considerable <br /> erosion of the valley edges and has deposited sediments continental in origin The <br /> Pliocene (5 - 2 million years ago), Pleistocene (2 million - 10,000 years ago) and <br /> Recent rocks consist mainly of semiconsolidated to unconsolidated claystones, <br /> sandstones and conglomerates, and contain most of the groundwater resources in the <br /> area <br /> Subsurface material encountered was alluvium to the total depth of each boring in <br />' the previous assessment The alluvium was characterized by low to moderate <br /> permeability, loose, light brown, very silty, very fine- to medium- grained sand <br /> (SM/ML) to a depth of 13 feet, overlying moderate to highly permeable, loose, dark <br /> brown, silty, fine- to medium- grained sand (SM) to a depth of approximately 27 feet <br /> Underlying this is a zone of consolidated, slight to moderate plasticity, medium dense, <br />' low permeability, gray brown, silty, organic clay (OH/ML) to a depth of 53 feet This <br /> clay zone was underlain by consolidated, slight to moderate plasticity, medium dense, <br /> low permeability, light brown, trace very fine sand, minor silt, clay (CH) to a depth <br /> EB-8lo1-3 9207-EO37 WP <br />
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