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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
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2008_29.tif
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EHD - Public
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few silt and clay interbeds. Contacts between these three subunits are not distinct <br /> and are therefore subject to interpretation. By their nature these sedimentary units <br /> interfinger and are discontinuous on an individual basis. <br /> 2.3.3 FAULTING AND SEISMICITY <br /> The Forward Landfill is located in an area of relatively low seismic activity. No <br /> evidence of Holocene-age faulting on the property has been found either <br /> through a review of available literature or through site investigations and the site <br /> in not within or near any State of California Earthquake Fault Zones (as <br /> mandated by the Alquist-Priolo Earthquake Fault Zoning Act passed in 1974 and <br /> updated through 1999). The nearest known fault to the site, the Tracy-Stockton <br /> Fault Zone, passes through the City of Stockton, 6.5 miles northwest of the site. <br /> This fault zone is the closest known to the landfill and does not show evidence of <br /> Holocene displacement. The nearest active fault is the Great Valley 7 fault <br /> located approximately 19.8 miles (31.9km) southwest of the site. <br /> The seismic exposure of FL was evaluated by Geologic Associates (2007). Since <br /> the Forward Landfill is a Class II facility, the landfill design is based on the <br /> anticipated peak horizontal ground acceleration (PHGA) from a Probabilistic <br /> Seismic Hazard Assessment (PSHA) approach or the Maximum Credible <br /> Earthquake (MCE). Therefore, GLA proposed the MCE magnitude of 6.7 on the <br /> Great Valley 7 fault as a design-level earthquake. <br /> Using this magnitude, GLA used a variety of attenuation relationships from Blake <br /> (2004a) to evaluate the PHGA at the site. The attenuation relationship by <br /> Campbell and Bozorgnia (1994, revised 1997) for alluvial sites assuming a <br /> reverse fault event was concluded to be the most appropriate for the site <br /> conditions. Using this attenuation relationship, a PHGA of 0.13g was calculated <br /> for the MCE event of 6.7 on the Great Valley 7 fault at a distance of 19.8 miles <br /> (31.9 km). However, the family of attenuation curves for reverse faulting <br /> (Ord6nez, 2006; SHAKE 2000) indicates an upper bound horizontal ground <br /> acceleration of 0.15g. <br /> Forward Landfill-Project Description 2-4 BRYAN A.STIRRAT&ASSOCIATES <br /> j:\Allied\Forward\2007.0018 Lateral Expansion\Reports\Proj Descrip\021308 Final Proj Des\Sec 2.doc:2/13/2008) <br />
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