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ARCHIVED REPORTS_2008_29
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ARCHIVED REPORTS_2008_29
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Last modified
7/17/2020 3:53:28 PM
Creation date
7/3/2020 10:54:10 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2008_29
RECORD_ID
PR0440005
PE
4433
FACILITY_ID
FA0004516
FACILITY_NAME
FORWARD DISPOSAL SITE
STREET_NUMBER
9999
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106001-3, 5
CURRENT_STATUS
01
SITE_LOCATION
9999 AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2008_29.tif
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EHD - Public
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the northern portion of the site. The North Creek was successfully relocated <br /> from its original location (south of the former Austin Road Landfill which is now <br /> part of FL) to the northern boundary of the FL in 2001/2002. <br /> 2.3 GEOLOGY AND SEISMICITY <br /> 2.3.1 REGIONAL GEOLOGY <br /> The Forward Landfill is located in the central portion of the Great Valley <br /> geomorphic province in the region locally referred to as the northern San <br /> Joaquin Valley. The Great Valley is an elongated asymmetrical structural trough <br /> bounded on the east by the Sierra Nevada and on the west by the Coastal <br /> Range. In the northern San Joaquin Valley, nearly 8,000 feet of sediments have <br /> accumulated within the basin, including an accumulation of about 5,250 feet of <br /> marine clays, silts, and sands subsequently overlain by approximately 2,500 feet <br /> of unconsolidated terrestrial sediments. The uppermost portion includes the <br /> Pleistocene age Victor Formation. In the northern San Joaquin Valley, this unit <br /> includes about 100 feet of laterally and vertically discontinuous fine grained clays <br /> and silts with interbedded coarser-grained sediments characteristic of <br /> meandering fluvial deposition. <br /> 2.3.2 SITE GEOLOGY <br /> The geology and hydrogeology of FL have been detailed in several reports <br /> including Kleinfelder & Associates (1991, 1997, 1999), CH2MHill (1992) Beta <br /> Associates (1988), EMCON Associates (1972), and GLA (2007). These studies <br /> confirm that the geology, as well as the hydrogeology of the FL, are consistent <br /> with regional conditions. <br /> The uppermost sediments of the Victor Formation have been divided into three <br /> subunits based on lithologic logs for boring and monitoring wells that identified <br /> logical groupings of gross lithology and pervasive color distinctions. The upper <br /> 28 to 40 feet consist of highly interbedded sandy silt, clayey silt, silt, and clay. <br /> Most of these sediments have an oxidized appearance and an orange brown <br /> color. Below this subunit is a 25-to 35-foot thick, gray- brown interbedded sand, <br /> silty sand, and minor clay subunit. The third subunit occurs to a depth of about <br /> 110 feet and is generally light brown to yellow brown dominated by fine to <br /> medium-grained sand, with some coarse-grained sand and gravelly layers and a <br /> Forward Landfill-Project Description 2-3 BRYAN A.STIRRAT&ASSOCIATES <br /> j:\Allied\Forward\2007.0018 Lateral Expansion\Reports\Prof Descrip\021308 Final Proj Des\Sec 2.doc:2/13/2008) <br />
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