Earthquake Hazard Mitigation Flashcards
What hazards are associated with earthquakes?
- Ground rupturing and slope failures
- Liquefaction
- Structural damage
Ground Dispacement
Rupturing of ground surfaces
Landslides
Slippage of large blocks of Earth along defined surfaces.
Liquefaction
The transformation of cohesive soil into a slurry of mud by seismic vibrations.
Tsunamis
Large sea waves produced by undersea landslides, asteroid impacts, volcanoes, or earthquakes.
How is seismic hazard assessed?
- Analysis of event frequency and intensity
- Stratigraphic anaysis
- Geomorphic analysis
- Tracking of crustal movement
What are the 3 components of seismic risk studies?
- Geologic studies
- Soil engineering studies
- Seismological studies
What are the 3 types of analysis of event frequency and magnitude?
- Historical earthquake frequency, location, and intensity
- Correlation of earthquakes with mapped faults
- Estimation of future seismic intensities with odds of reccurence
4 Components of Stratigraphic Analysis
- Foundation soils and their shaking susceptibility
- Slope instability and subsidence
- Fault types and activity within 100 km
- Location of landslides, ground settlement, and water inundation problems
4 Components of Geomorphic Aanalysis
- Foundation soils and their shaking susceptibility
- Slope instability and subsidence
- Fault types and activity within 100 km
- Location of landslides, ground settlement, and water inundation problems
Tracking of Crustal Movement
Regional tectonics and patterns of deformation
What can be done to reduce seismic risk?
- Structural design
- Land use planning and zoning
- Emergency management
Can earthquakes be predicted?
Seismic forecasting is possible, but not prediction of a single event.
How are earthquakes forecasted? (4 ways)
- Detection of precursor (foreshocks)
- Location of seismic gaps
- Tracking migrating earthquakes
- Determining historic and prehistoric seismicity
How does seismic activity correspond to tectonic setting? (2 ways)
- Activity at plate boundaries
2. Intraplate earthquakes