1.12 Shaking & Stirred Flashcards
P Waves
Short wavelength & travels fast through both solid rock and liquid, waves push and pull creating compressional and extensional zones.
S Waves
Slower than P waves but can only move through solid and rock, longer wavelength and movement is perpendicular to direction of travel.
L Waves
Slowest, most destructive wave and can only move across surface, largest amplitude and shakes ground horizontally as the wave travel forward.
Crustal Fracturing
Energy released causes crust to crack and land to be displaced vertically.
Ground Shaking
Causes buildings, bridges, roads and other infrastructure to collapse.
Liquefaction
Surface rocks lose strength in violent shaking and become more liquid than solid thus losing its ability to support building foundations and cars.
Landslides
Shaking places rock slopes under increased stress which could lead to failure.
Secondary Hazards
Indirect EQ causes i.e. liquefaction and landslides.
Aftershocks
Smaller earthquakes that follow main earthquake, whilst fault readjusts to initial release of strain - these can significantly hamper response and recovery especially when larger than expected.