Divergent plate boundaries
Transform plate boundaries
Plates slide horizontally; locked at irregularities in plate boundaries
Convergent plate boundaries
The energy required to move plates is released as
large earthquakes
Spreading Center Earthquakes: Iceland
Red Sea and Gulf of Aden
Subduction-zone earthquakes
Deep earthquakes:
Subducting plate generates earthquakes to 700km in depth
- Earthquake energy dissipates before reaching the surface
Seismic-Gap Method
Subduction-Zone Earthquakes: Indonesia, 2004
Subduction-Zone Earthquakes: Mexico City, 1985
Resonance:
- 5,700 buildings damaged, 15% collapsed
- Small towns near epicenter had much less damage
- Seismic resonance amplified ground motion due to soft, unconsolidated lake-sediment
- T < 10s waves
- Weak building code enforcement
- 6-16 story buildings resonate to destruction
Pacific Northwest: The Upcoming Earthquake
Pacific Northwest: Earthquake in 1700, The Trees Tell the Story
Transform-Fault Earthquakes: Haiti, 2010
Transform-Fault Earthquakes: Turkey, 1999
Transform Fault EQs: San Andreas
San Andreas Fault: different sections behave differently:
San Andreas Fault: Bay Area EQ Probabilities