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SU0004094
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Last modified
10/27/2020 1:02:10 PM
Creation date
9/6/2019 10:43:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004094
FACILITY_NAME
QX-01-0002
STREET_NUMBER
36736
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36736 S KOSTER RD
RECEIVED_DATE
1/8/2002 12:00:00 AM
QC Status
Approved
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\MIGRATIONS\K\KOSTER\36736\QX-01-02_PA-0200065\SU0004094\EIR 2004.PDF
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EHD - Public
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4.Environmental Analysis <br /> Seismic Hazards <br /> The proposed project site could experience the effects of a major earthquake from one of the <br /> active or potentially active faults located in proximity to the project site. The four major hazards — <br /> associated with earthquakes are fault surface rupture(ground displacement),ground shaking, <br /> ground failure, and settlement. This EIR considers the potential for hazards associated with <br /> ground shaking,earthquake-induced slope failure(landslides), liquefaction and settlement but <br /> does not further discuss surface fault rupture. Surface fault rupture is not discussed because no <br /> active faults capable of generating surface rupture are located beneath the proposed project site. <br /> Seismic Ground Shaking <br /> Earthquakes in the San Francisco Bay and San Joaquin Valley Region could produce strong — <br /> ground shaking in the project area. Ground-shaking intensity is related to the size(i.e., <br /> magnitude)of an earthquake, the distance to the site, and the response of the geologic materials <br /> that underlie the site. As a rule, the greater the earthquake magnitude and the closer the fault — <br /> rupture to the site,the greater the intensity of ground shaking. Violent shaking is generally <br /> expected at and near the epicenter of a large earthquake, although studies of recent earthquakes, <br /> such as those conducted after the 1992 Landers earthquake, indicate that directional ground — <br /> motion along a fault can cause strong ground shaking farther away from the epicenter. Seismic <br /> hazards due to ground shaking can cause the greatest amounts of damage to structures and <br /> utilities and unsecured equipment. <br /> In 1999,California Geological Survey completed the Seismic Shaking Hazard Maps for <br /> California to describe the statewide distribution of estimated ground motion through the state. — <br /> These maps provide a conservative estimate, through probabilistic analysis, of the peak ground <br /> acceleration for all regions of California. Based on estimates of this seismic hazards assessment, <br /> peak ground acceleration in the region of the proposed project site could reach or exceed 0.3 to <br /> 0.4g(CGS, 2003a).6.,7 Seismic ground shaking is discussed further in the Impacts and Mitigation <br /> section of this chapter. <br /> 6 A probabilistic seismic hazard map shows the hazard from earthquakes that geologists and seismologists agree <br /> could occur.It is"probabilistic in the sense that the analysis takes into consideration the uncertainties in the size <br /> and location of earthquakes and the resulting ground motions that can affect a particular site.The maps are typically <br /> expressed in terms of probability of exceeding a certain ground motion.For example,the 10 percent probability of <br /> exceedance in 50 years maps depicts an annual probability of 1 in 475 of being exceeded each year.This level of <br /> ground shaking has been used for designing buildings in high seismic areas.The maps for 10 percent probability of <br /> exceedance in 50 years show ground motions that geologists and seismologists do not think will be exceeded in the <br /> next 50 years.In fact,there is a 90 percent chance that these ground motions will not be exceeded.This probability <br /> level allows engineers to design buildings for larger ground motions that geologists and seismologists think will <br /> occur during a 50-year interval,which makes buildings safer than if there were only designed for the ground <br /> motions that are expected to occur in the next 50 years.Seismic shaking maps are prepared using consensus <br /> information on historical earthquakes and faults.These levels of ground shaking are used primarily for formulating <br /> building codes and for designing buildings.The maps can also be used for estimating potential economic losses and <br /> preparing for emergency response(Peterson et al., 1999). <br /> 7 The damage level represents the estimated overall level of damage that will occur for various MMI levels.The _ <br /> damage,however,will not be uniform.Some buildings will experience substantially more damage than this overall <br /> level,and others will experience substantially less damage.Not all buildings perform identically in an earthquake.The <br /> age,material,type,methal of construction,size,and shape of a building all affect its performance(ABAG, 1998). <br /> RMC Pacific Vernalis Quarry Mining and Reclamation Project 4.7-10 ESA 1203015 <br /> Draft Environmental Impact Report May 2006 <br />
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