HR: 08:45h
AN: S31C-04 [Abstracts]
TI: Assessing Seismic Hazards - Algorithms, Maps, and Emergency Scenarios
AU: * Ferriz, H
EM: hferriz@geology.csustan.edu
AF: California State University Stanislaus, 801 W. Monte Vista Ave., Turlock, CA 95382, United
States
AB:
Public officials in charge of building codes, land use planning, and emergency response need sound estimates
of seismic hazards. Sources may be well defined (e.g., active faults that have a surface trace) or diffuse (e.g., a
subduction zone or a blind-thrust belt), but in both cases one can use a deterministic or worst-case scenario
approach. For each scenario, a design earthquake is selected based on historic data or the known length of
Holocene ruptures (as determined by geologic mapping). Horizontal ground accelerations (HGAs) can then be
estimated at different distances from the earthquake epicenter using published attenuation relations (e.g.,
Seismological Res. Letters, v. 68, 1997) and estimates of the elastic properties of the substrate materials. No
good algorithms are available to take into account reflection of elastic waves across other fault planes (e.g., a
common effect in California, where there are many strands of the San Andreas fault), or amplification of waves in
water-saturated alluvial and lacustrine basins (e.g., the Mexico City basin), but empirical relations can be
developed by correlating historic damage patterns with predicted HGAs. The ultimate result is a map of HGAs.
With this map, and with additional data on depth to groundwater and geotechnical properties of local soils, a
liquefaction susceptibility map can be prepared, using published algorithms (e.g., J. of Geotech. Geoenv. Eng., v.
127, p. 817-833, 2001; Eng. Geology Practice in N. California, p. 579-594, 2001). Finally, the HGA estimates,
digital elevation models, geologic structural data, and geotechnical properties of local geologic units can be used
to prepare a slope failure susceptibility map (e.g., Eng. Geology Practice in N. California, p. 77-94, 2001).
Seismic hazard maps are used by: (1) Building officials to determine areas of the city where special construction
codes have to be implemented, and where existing buildings may need to be retrofitted. (2) Planning officials to
evaluate plans for new growth (though in most cities land use patterns are historically established). (3)
Emergency response officials to plan emergency operations. (4) Insurance commissioners to estimate losses
and insurance claims (e.g., with FEMA's software HAZUS).
DE: 7200 SEISMOLOGY
DE: 7212 Earthquake ground motions and engineering seismology
DE: 7223 Earthquake interaction, forecasting, and prediction (1217, 1242)
SC: Seismology [S]
MN: 2007 Joint Assembly